MINERALOGY
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  20040156 Bai Wenji (Institute of Geology, Chinese Academy of Geological Sciences , Beij ing); Yang jingsui An Unusual Mantle Mineral Group in Ophiolites of Tibet, Chin a (Geology in China, ª©ISSNªª1000-3657, ª©CNªª11-1167/P, 30(2), 2003, p. 144-150, 6 ª©illus.ªª, 23 ª©refs.ªª)ª¤
Keywords: ophiolite Tibet
  An unusual mantle mineral group consisting of more than 100 species (or subsp ecies) minerals was discovered in chromite from the Yarlung Zangbo ophiolite bel t, Tibet. It includes native element minerals alloys, oxides (arsenides) and sil icates. According to experimental data, some of the minerals are ultrahigh-press ure minerals, possibly formed at the Earth's core-mantle boundary, and are the p roducts of chemical reactions between liquid iron of the Earth's outer core and silicates at the base of the lower mantle; others might be derived from the lowe r mantle, transitional zone and upper mantle. The mantle mineral group in Tibet has great significance in mineralogy and geodynamics.

ª¤20040157 Bi Shu (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Gua ngzhou, Guangdong); Xie Xiande Mineralogical Characteristics of Tons tein in Sou thwestern Shandong Province and its applications (Geochimica, ª©ISSNªª03 79-1726, ª©CNªª 44-1398/P, 32(3), 2003, p.291-296, 8 ª©illus.ªª, 5 tables, 6 ª©refs.ªª, with Eng lish abstract)
Keywords: coal gangue

   20040158 Cao Mingli (School of Resources and Environmental Engineering , Wuhan Universi ty of Technology, Wuhan, Hubei); Yu Yongfu Preparation and Propertie s of Al-Pil lared Interlayer Montmorillonite (Journal of China University of Mining & Techn ology, ª©ISSNªª1000-1964, ª©CNªª32-1152/TD, 32(4), 2003, p.416-418, 432, 3 ª©ill us.ªª, 1 table, 10 ª©refs.ªª, with English abstract)ª¤
Keywords: ben tonite deepening processing

   20040159 Chen Jieyu (Test Center, China University of Geosciences, Wu han, Hubei); Yan Chunjie A Method for Rapid Preparation of Hydrazine-Kaolinite Inter calation Co mplex and its Significance (Acta Petrologica et Mineralogica, ª©ISSNªª1 000-6524, ª©CNªª11-1966/P, 22(1), 2003, p.99-102, 3 ª©illus.ªª, 17 ª©refs.ªª)ª¤
Keywords: kaolinite X-ray diffraction analysis scanning electron m icroscopy ª¥
  Grinding the mixture of kaolin and hydrazine concentrate can not only raise t he speed of intercalation so that the intercalation rate reaches 96 % in 10 minu tes, but also greatly improve the refining of kaolin. When the complexes are hea ted to 120 ¡æ, the gas they send out can further delaminate kaolin. In this way, the authors can get the refined kaolin whose grain size is -2¡¡¦Ìm>90%, and the lamellar crystal is perfect. This technology offers an innovational thinking and a method for preparing ¡°double 90¡± refine kaolin.


ª¤ª¤20040160 Cheng Hao (Department of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui); Chen Daogong Laser-Raman Spectro scopy and L AM-ICP-MS Study of Zircons from Huangtuling, Hubei Province, China (Eart h Scien ce Frontiers, ª©ISSNªª1005-2321, ª©CNªª11-3370/P, 10(2), 2003, p.313-317, 3 ª©il lus.ªª, 1 table, 17 ª©refs.ªª, with English abstract)ª¤
Keywords: gr anulites pb-pb dating Hubei Province ª¥

   20040161 Ding Zhenhua (Institute of Geochemistry, Chinese Academy of S ciences, Guiyang , Guizhou); Zheng Baoshan Discovery of A Hg-, Zn-, S-Bearing Mineral in Coal ( Geology-Geochemistry, ª©ISSNªª1008-0244, ª©CNªª52-1044/P, 31(2), 2003, p.87-89, 1 ª©illus.ªª, 2 tables, 12 ª©refs.ªª, with English abstract)ª¤ Keywor ds: coal toxic materials

  20040162 Feng Xuwen (No.2 Institute of Oceanography, State Oceanic Adm inistration, Han gzhou, Jiangsu); Qian Jiangchu Study of Phase Change of 1nm Manganat e in Polyme tallic Nodules and its Main Controlling Factors (Acta Mineralogica Sinic a, ª©ISSNªª 1000-4734, ª©CNªª52-1045/P, 23(2), 2003, p.109-114, 3 ª©illus.ªª, 1 table, 23 ª© refs.ªª)ª¤
Keywords: polymetal crust manganese minerals
  It is found that more or less 1nm manganate in polymetallic nodules can be ch anged into 0.7 nm manganate after dried or heated at room temperature for 5 hour s. This could be inferred that the 0.7nm manganate in the nodule is not the orig inal mineral phase but only the product of phase change from the 1nm manganate. also found that there is a positive correlation between the structural stabilit y of 1nm manganate and the volume of cations in the structure. ª¤

ª¤20040163 Gao Xiang (School of Earth and Space Science, Peking Univers ity, Beijing); L u Anhuai Refinement of Crystal Unite Cell Parameters of Native Crypt omelane in the Supergene Oxidation Zone of Xiangtan Manganese Deposit, Hunan Province, China (Acta Petrologica et Mineralogica, ª©ISSNªª1000-6524, ª©CNªª11-1966/P , 22(1), 2003, p.77-79, 2 tables, 25 ª©refs.ªª)ª¤
Keywords: cryptome lane manganese deposits Hubei Provinceª¥
This paper is mainly devoted to the refinement of the crystal unit cell param eters of the native manganese oxide from the supergene oxidation zone of the Xia ngtan manganese deposit, Hunan Province. With the computer programs of Rietveld- DBW 9411 and Pirum, it is revealed that the body-centered monoclinic cryptomelan e is the main phase of the mineral. It is also pointed out that the troubles of refining are caused by the extreme difficulty in finding a single crystal partic le and by the XRD pattern characterized by broadening, relatively high backgroun d and asymmetry.


ª¤20040164 Guo Ying (School of Geology, China University of Geosciences, Beijing); Pan Z haolu Colorimetric Characteristics and Evaluation of Same Color with Different Spectrum of Green Jadeite (Mineral Resources and Geology, ª©ISSNªª1001-5 663, ª©CNªª45-1 174/TD, 17(2), 2003, p.173-176, 2 ª©illus.ªª, 3 tables, 8 ª©refs.ªª, with Englis h abstract)ª¤
Keywords: jadeite ª¤

   20040165 Guo Ying (College of Mineral and Engineering, China Universit y of Geosciences , Beijing); Lai Xingyun Atomic Force Microscopy of Plastic Deformati on Characte ristics of Jadeite (Acta Mineralogica Sinica, ª©ISSNªª1000-4734, ª©CNªª5 2- 1045/P, 23(2), 2003, p.158-162, 4 ª©illus.ªª, 10 ª©refs.ªª, with English abstrac t)ª¤
Keywords: jadeite plastic deformation

ª¥ 20040166 Hu Xiaoqiang (Department of Geosciences, Chengdu University o f Technology, Ch engdu, Sichuan); Chen Hongde Assortment of Biological Fabric of Ore Minerals ( Geology and Prospecting, ª©ISSNªª0495-5331, ª©CNªª11-2042/P, 39(3), 2003, p.31-3 4, 14 photos, 1 table, 11 ª©refs.ªª)
Keywords: metal deposits
  The assortment of biological fabrics of ore minerals is discussed. The fabric s can be divided into two types:1) the organic colloid fabric of ore minerals, w hich was formed by the direct mineralization of organism; 2) the organic replace ment biological fabric of ore minerals, which was formed by the indirect mineral ization of organism. The biological fabric can also be sort into the biological structure and the biological constitution. The authors describe the characterist ics of each sort of biological fabrics of ore minerals by typical examples.


ª¤20040167 Huang Fengming (Gemmological Institute, China University of G eosciences, Wuha n, Hubei); Liu Huifang Physical Properties and Origins of Synthetic and Diffuse d Star Corundum (Earth Science¡ª¡ªJournal of China University of Geoscie nces, ª©ISSNªª 1000-2383, ª©CNªª42-1233/P, 28(3), 2003, p.255-260, 4 ª©illus.ªª, 2 tables, 15 ª©refs.ªª, with English abstract)
Keywords: corundum deposits

ª¤20040168 Jiang Yonghong (School of the Earth Sciences and Land Resourc es, China Univer sity of Geosciences, Beijing); Li ª©Shengrongªª The Typomophism of P yrite of Jincha ng Gold Deposit in Mojiang County, Yunnan Province, China (Journal of Mi neralog y and Petrology, ª©ISSNªª1001-6872, ª©CNªª51-1143/TD, 23(2), 2003, p.22-26, 3 ª© illus.ªª, 4 tables, 7 ª©refs.ªª, with English abstract)ª¤
Keywords: gold deposits pyrite Yunnan Province


  20040169 Li Xiaofeng (Institute of Mineral Resources, Chinese Academy of Geologi cal Sciences, Beijing); Hua Renmin The Influence of Rock Deformation on the Cry stallinity of Clay Minerals: A Case Study of the Jinshan Gold Deposit in Jiangxi Province, China (Acta Petrologica et Mineralogica, ª©ISSNªª1000-6524, ª©CNªª1 1-1966/P, 22(3), 2003, p.265-272, 2 ª©illus.ªª, 3 tables, 60 ª©refs.ªª)
Keywords: illite chlorite water-tock interaction Jiangxi Province
ª¥Being products of water-rock interaction during the migration of fluids, clay minerals can help to understand the mechanism of water-rock interaction and fea tures of fluids. With the Jinshan gold deposit in Jiangxi Province as an example , the authors determined the crystallinity, mean crystal size and lattice strain of illite and chlorite and, on such a basis, discussed the difference of crysta llinity, mean crystal size and lattice strain between illite and chlorite caused by deformation of mylonite and untramylonite. The relationships between crystal linity and crystal size of illite or chlorite can reflect the behavior and mecha nism of deformed rock.
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  20040170 Li Yi (Department of Resources and Environment, Guangxi Norma l University, Gu ilin, Guangxi); Lai Lairen Preliminary mineralogical Study of Scorod ite (Miner al Resources and Geology, ª©ISSNªª1001-5663, ª©CNªª45-1174/TD, 17(2), 2003, p.17 0-172, 2 ª©illus.ªª, 2 tables, 2 ª©refs.ªª, with English abstract)ª¤ Keywords: scorodite ª¥

ª¤ 20040171 Liu Xiaodong (State Key Laboratory of Mineral Deposits Resear ch, Nanjing Univ ersity, Nanjing, Jiangsu); Hua Renmin Cathodoluminscence Study of Ap atite in Go ld-Bearing Quartz Vein from Bitan Au-Ag-Cu Deposit (Acta Mineralogica Si nica, ª©ISSNªª 1000-4734, ª©CNªª52-1045/P, 23(2), 2003, p.129-135, 6 ª©illus.ªª, 1 table, 24 ª© refs.ªª, with English abstract)
Keywords: gold deposits apatite luminescence analysis Fujian Province ª¥ª¤

  20040172 Liu Yan (China University of Geosciences, Beijing); Gao Yan Mineralogical Ch aracteristics of Keketuohai Cat's-Eye Aquamarine in Xinjiang and its Exploration (Geology and Prospecting, ª©ISSNªª0495-5331, ª©CNªª11-2043/P, 39(3), 20 03, p.25-30, 2 ª©illus.ªª, 6 tables, 9 ª©refs.ªª)ª¤
Keywords: beryl Xinjiang ª¥
 Cat's-eye aquamarine as a very special species among beryls and has a high va lue. The cat's-eye appears because there are many gas-liquid inclusions array in a certain direction. A lot of light green, light yellow and light blue cat's-ey e aquamarine has been found in Keketuohai, Xinjiang. According to the detailed a nalyses and examinations of X-ray, micro-hardness test, infrared spectrum, Raman spectrum etc., chemical and physical characteristics, inner structure, inclusio n distribution and compositions, and the OH state were systemically studied. The e studies have important significances for the application and exploit of this m ineral. Irradiation and heat-treatments of cat's-eye aquamarines have also been studied.

  20040173 Long Yongzhen (Department of Geology, Central-South Universit y, Changsha, Hun an); Dai Tagen Mineralogy of Bauxite Ore at Longhua, guangxi Provinc e, China ( Geology-Geochemistry, ª©ISSNªª1008-0244, ª©CNªª52-1044/P, 31(1), 2003, p.74-77, 2 ª©illus.ªª, 2 tables, 2 ª©refs.ªª)ª¤
Keywords: bouxite Guangxi Pr ovince
 The Longhua bauxite deposits is a diaspore deposit. The major mineral is dias pore and the secondary minerals are gibbsite, bochmite, kaolinite, illite, chamo site, anatase, rutile, hematite and lithiophorite. Aluminum, the major element i n the ore, is distributed evenly. This kind of ore is suitable for high-pressure Bayer processing. In the bottom mud of the deposit, a mineral unknown in this d istrict was determined as beidellite by means of XRD and Greene-Kelly (1953), an d it accounts for 15.45% as revealed by montmorillonite-group quantitative analy sis (Jones, 1964).
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  20040174 Luo Taiyi (Institute of Geochemistry, Chinese Academy of Scie nces, Guiyang, G uizhou); Li Xiaobiao Sasaite from Niutitang Black Shales, Zunyi, Gui zhou Provin ce, China (Acta Mineralogica Sinica, ª©ISSNªª1000-4734, ª©CNªª52-1045/P, 23(3), 2003, p.205-210, 4 ª©illus.ªª, 6 tables, 6 ª©refs.ªª)ª¤
Keywo rds: variscite carbonaceous shale Guizhou Provincez ª¥
  Sasaite from Niutitang black shales at Zunyi occurs mainly as micro-fissures in Ni-Mo multi-metal mineralization strata, and also as small sasaite veins in b lack shales beneath the Ni-Mo multi-metal mineralization strata. Ir spectra, DG- TGA, TEM and chemical composition of the sasaite have been determined, and relat ive crystal cell parameters have been calculated from the XRD data; the differen ce between sasaite and vashegyite has been discussed in this paper. Part of stru cture water in sasaite is easy to lose, leading to a variety of XRD spectra, and steady XRD spectra can be kept after the samples have been preserved for long u nder natural conditions.


ª¤ª¤20040175 Lu Haiping (Department of Earth Sciences, Nanjing University, Nanjing, Jiangs u); Wang Rucheng Structural and Chemical Stability of Zircon: Study of Nuclear- Waste Disposal Aanlogous Mineral (Earth Science Frontiers, ª©ISSNªª1005- 2321, ª©CNªª11- 3370/P, 10(2), 2003, p.403-410, 1 ª©illus.ªª, 1 table, 53 ª©refs.ªª, with Englis h abstract)ª¤
  Keywords: radioactive waste waste disposal zircon ª¥

ª¤20040176 L¨¹ Zhicheng (Institute of Geochemistry, Chinese Academy of Sc iences, Guiyang, Guizhou); Duan Guozheng Mineral Chemistry of Biotite from Granites Associated with Different Mineralization in Three Stages of Yanshanian Period in the Southe rn-Middle parts of the Great Hinggan Mountains and its Petrogenetic and Metallog enic Significance, Northeast China (Acta Mineralogica Sinica, ª©ISSNªª10 00-4734, ª©CNªª 52-1045/P, 23(2), 2003, p.177-184, 2 ª©illus.ªª, 2 tables, 10 ª©refs.ªª, with En glish abstract)ª¤
Keywords: granites biotite Great Hinggan Mountia ns China

  20040177 Ni Zhiyao (College of Earth Sciences, Chengdu University of T echnology, Cheng du, Sichuan); Wang Renmin ª©ª¬ª©207ªª[KG1]Pbªª/ª¬ª©206ªªPb Age of Zi rcon and ª¬ª©40ªª[KG*2/3]Ar/ª¬ª©39ªªAr of Am phibole from Plagioclase Amphibolite in the Taihua Group, Luoning, Henan Provinc e, China (Geological Review, ª©ISSNªª0371-5736, ª©CNªª11-1952/P, 49(4), 2003, p.361-366, 4 ª©illus.ªª, 3 tables, 29 ª©refs.ªª, with English abstract)ª¤
Keywords: amphibolites Pb-Pb dating Ar-Ar dating Henan Province

  20040178 Nie Fenglian (Gold Geological institute of CAPF, Langfang, He bei); Zhao Tianx in Characteristics of Gold Mineral and Geological Significance of Go ld Fineness of Some Gold Deposits in Eastern Hebei Province, China (Gold Geology, ª©ISSNªª1006 -558X, ª©CNªª11-3623/TD, 9(1), 2003, p.48-51, 2 ª©illus.ªª, 2 tables, 3 ª©refs. ªª)
Keywords: gold deposits gold minerals Hebei Province ª¥
  The Sanjiazi and Banbishan gold deposit of Qinglong area are occurred in the old metamorphic rocks. The main gold-carrying minerals are quartz and pyrite. Au rum is occurred mainly as cranny aurum, inclusion aurum and crystal detect aurum . The contrast of gold fineness shows that the older the metallogenetic epoch wa s, the higher the fineness of gold is: the forming temperature and the fineness of gold is in positive correlation, the deeper the gold deposit is, the higher t he fineness of gold is, the metallogenetic epoch of the Sanjiazi gold deposit is younger and it had gone through several times ore-forming process, it's a middl e to mid-high-temperature deposit. The Banbishan gold deposit has older metallog enetic epoch and its a high-mid-temperature deposit.
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  20040179 Peng Suping (Department of Resources Exploration Engineering, China Universit y of Mining and Technology, Beijing); Ding Shuli Discovery and chara cteristics of the Rare Mineral¡ª¡ªVaterite in Oil-Pumping Oil Well (Acta Mineralogi ca Sinica , ª©ISSNªª1000-4734, ª©CNªª52-1045/P, 23(1), 2003, p.45-50, 3 ª©illus.ªª, 4 tabl es, 33 ª©refs.ªª)
Keywords: calcite ª¥
  The scale that precipitated in ASP-driven pump oil well is a very serious pro blem in oil production in Daqing oil field of China. The growth of scale often d amages the drilling machine and increases the production cost. The study on XRD, IR, SEM and chemical analysis of scale show that the chemical composition of sc ale are mainly CaO and SiOª­2, which account nearly for 67% separately. A rare m ineral, vaterite, was found in the scale, which is a tiny crystal, often in the form of crystallite aggregates and usually associated with amorphous SiOª­2. It is suggested that the dissociated SiOª­2 and organic matter in pump oil well pla y an important role in the formation of vaterite.


ª¤ª¤20040180 Ren Yufeng (School of Materials Science and Engineering, Chin a University of Geosciences, Beijing); Ma Hongwen Synthesis of Gold-Tailing Geopolym ers and Inf luential Factors (Rock and Mineral Analysis, ª©ISSNªª0254-5357, ª©CNªª1 1-2131/TD, 22(2), 2003, p.103-108, 6 ª©illus.ªª, 1 table, 14 ª©refs.ªª)ª¤ Keywords: met akaolin
   This paper systematically discussed the relationships between t he compressive strength and the influential factors during geopolymerization of the gold-taili ng geopolymers. The samples were synthesized from 80% gold-tailing, 20% metakaol in and 10 mol/L NaOH or KOH solution. It was found that the compressive strength of the geopolymers was enhanced by raising temperatures strength of the samples increased continuously with increase of staying time in air, which is related t o obtaining water from air. et al. It was proved that fillings participated in g eopolymerization although they were much lower in solubility than metakaolin in alkaline solutions. And it was found that the geopolymers containing more potass ium feldspars had higher compressive strength than those with quartzes or contai ning fewer potassium feldspars.


ª¤ª¤20040181 Sun Ni (Earth and Space Science College, Peking University, Beijing ); Cui Wenyuan Mineralogical Characteristics and Genesis of Shousha n Stone in Jialiangshan, Fujian Province, China (Acta Petrologica et Mi neralogica, ª©ISSNªª1000-6524, ª©CNªª11-1966/P, 22(3), 2003, p.273-278, 3 ª©illu s.ªª, 4 tables, 11 ª©refsªª.)ª¤
Keywords: agalmatolite Fujian Province
  The authors have extensively studied Shoushan Stone from Jialiangshan in Fuji an Province based on such analytical means as EMPA, chemical analysis, XRD, IR a nd LRM. The results show that Shoushan Stone in Jialiangshan area is a kind of r ock mainly composed of pyrophyllite, diaspore and quartz. Most of the stones hav e perfect 2M type of pyrophyllite. The Shoushan Stone in Jialiangshan area was f ormed by hydrothermal activities and the ore-forming process can be divided obvi ously into three stages. The metallogenic temperature is about 285-405 degree an d the ore-forming pressure is lower than 0.26 GPa.
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  20040182 Wang Hongtao (Department of Earth Sciences, Nanjing Universi ty, Nanjing, Jia ngsu); Ji Junfeng An Experimental Study on Defluoridation of Drinkin g Water wit h Montmorillonite[WT][ST] (Acta Petrologica et Mineralogica, ª©ISSNªª1000-6524, ª©CNªª11-1966/P, 22(1), 2003, p.71-73, 76, 2 tables, 21 ª©refs.ªª)ª¤ Keywords: montmorillonite
  Montmorillonite adsorption experiments were conducted in the fluoride solutio n. The results show that an excellent negative correlation exists between the ad sorption ability of montmorillonite and pH values of the solution. Montmorilloni te adsorbs large quantities of fluorine ions and the defluoridation effect is re markable at low pH value. With the rising of the pH value, the amount of fluorin e adsorbed by montmorillonite decreases rapidly and, what is worse, montmorillon ite seems almost not to absorb fluorine ions at all in basic-neutral solution. T he amount of montmorillonite and the concentration of fluoride solution also aff ect the amount of fluorine adsorbed on montmorillonite.


ª¤ª¤20040183 Wang Jian (Guangzhou Institute of Geochemistry, Chinese Acade my of Sciences, Guangzhou, Guangdong); Li Jianping Ti-Bearing Diopsides from Cenozo ic Kamafugi tes in Western Qinling, Lixian County, Gansu Province, China (Acta Miner alogica l Sinica, ª©ISSNªª1000-4734, ª©CNªª52-1045/P, 23(2), 2003, p.115-123, 6 ª©illus. ªª, 2 tables, 23 ª©refs.ªª, with English abstract)ª¤
Keywords: melil itite diopside Qinliang Mountains

ª¥ª¤ 20040184 Yang Ji (Earth Sciences and Land Resources College of Chang'a n University, Xi 'an, Shaanxi) Discussion on the Relationships Between the ¡°Core¡± o f Mineral and the Physical-Chemical Property of Diamond (Guangdong Geology, ª©ISSNªª1 001-8670, ª©CNªª44-1201/P, 18(1), 2003, p.26-29, 4 ª©refs.ªª)ª¤
Keywo rds: diamond color centers
  This paper deals with the mechanism of formation of the electron-hole ¡°core¡± of mineral (diamond), and the effect of ¡°core¡± on the physical-chemical proper ty of diamond. The author believes that the hole core produced from heterovalent i somorphism makes it possible for the diamond to have a high thermal conductivity and electric conductivity. In other words, the electric conductivity of diamond is caused by the hole core.


ª¤ª¤20040185 Yang Zhijun (Department of Geosciences, Zhongshan University, Guangzhou, Guan gdong); Peng Mingsheng The UHF Analysis of Lattice Hydrogen in Diamo nd (Acta M ineralogica Sinica, ª©ISSNªª1000-4734, ª©CNªª52-1045/P, 23(2), 2003, p.149-152, 1 ª©illus.ªª, 1 table, 12 ª©refs.ªª, with English abstract)ª¤
Keywords: diamond lattice hydrogen ª¥

ª¤ 20040186 Zhang Aicheng (Department of Earth Sciences and State Key Lab oratory for Mine ral Deposits Research, Nanjing University, Nanjing, Jiangsu); Wang Rucheng Tapi olite from the Koktokay No.3 Rare Metal Granitic Pegmatite Dyke, Altai, Xinjiang Autonomous Region, China (Geological Journal of China Universities, ª©I SSNªª1006-7 493, ª©CNªª32-1440/P, 9(2), 2003, p.268-272, 2 ª©illus.ªª, 1 table, 13 ª©refs.ªª , with English abstract)ª¤
Keywords: tantalum deposits tapiolite i ron deposits manganese deposits Xinjiang

ª¤ 20040187 Zhang Shugen (College of Earth Science and Environmental Engi neering Central South University, Changsha, Hunan); Liu Chunbo Study on Mineralogica l Character istics of Coal Gangue in the Central Area of Hunan Province, China (Huna n Geolo gy, ª©ISSNªª1001-4756, ª©CNªª43-1147/P, 22(2), 2003, p.96-100, 86, 2 ª©illus.ªª, 6 photos, 6 tables, 14 ª©refs.ªª)ª¤
Keywords: coal gangue Hunan Province
  This paper studied the mineralogical characteristics of coal gangue in the ce ntral area of Hunan Province by way of chemical analysis, mineral and rock ident ification, X-ray diffraction analysis, scanning electron miroscopic analysis, as certained the chemical compositional compositional characteristics, mineral comp ositional characteristics, and crystalline characteristics of the kaoliniter, se riciter, on the base of which the authors simply classified the coal gangues and pointed out the utilize directions.


ª¤ª¤20040188 Zhao Liang (Institute of Surfacial Geochemistry, Nanjing Univ ersity, Nanjing, Jiangsu); Ji Junfeng Chemical Weathering of Chlorite in Chinese Loe ss-Paleosol Sequences in the last 130 Ka and Climate Change (Acta Mineralogica Sini ca, ª©ISSNªª 1000-4734, ª©CNªª52-1045/P, 23(2), 2003, p.163-168, 5 ª©illus.ªª, 1 table, 18 ª© refs.ªª, with English abstract)
Keywords: paleoclimatology Upper Pleistocene(Loess Plateau China

ª¤ 20040189 Zhao Xingyuan (Research Institute of Petroleum Exploration and Deve lopment, PetroChina, Beijing) Conditions for Formation of Kaolonite Subgroup in Tarim Basin, Xinjiang, China (Xinjiang Petroleum Geology, ª©ISSNªª1001-3873, ª©CNªª65-1107/TE, 24(5), 2003, p.419-423, 3 ª©illus.ªª, 1 pla te, 1 table, 5 ª©refs.ªª)ª¤
Keywords: kaolinite Tarim Basin Xinjiang
  Kaolinite subgroup is found in Tarim Basin as kaolin and dickite pieces, both have individual feature and forming condition. The authigenic kaolinite occurre d in Lower Jurassic, Triassic, Carboniferous sand-shale member and Kela No.2 gas structural zone, allothigenous kaolinite appeared in Lower Ordovician limestone cracks. The dickite is found in Carboniferous sandstone of Mincan No.1 Well in southern Tarim. According to mineral features of kaolinite and dickite, the sedi mentary environments of these horizons and water media at stage of hydrocarbon a ccumulation are analyzed in this paper.
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  20040190 Zhao Xingyuan (Research Institute of Petroleum Exploration an d Development, P etroChina, Beijing) Characteristics and Formation of Attapulgite in Tarim Basi n, Xinjiang, China (Xinjiang Petroleum Geology, ª©ISSNªª1001-3873, ª©CN ªª 65-1107/TE, 24(3), 2003, p.214-217, 3 ª©illus.ªª, 2 tables, 1 plate, 2 ª©refs.ªª )ª¤
Keywords: palygorskite Tarim Basin Xinjiang
  Attapulgite is of certain mineralogical features in chemical composition, X-r ay diffraction and infrared spectrum. In Tarim Basin, it is primarily distribute d in Palaeogene, secondly in Cretaceous and Neogene. The formation is closely re lated to these geological factors such as arid-semi arid paleo-climate and water medium enriched with magnesian ions.


ª¤ª¤20040191 Zhu Jianxi (Guangzhou Institute of Geochemistry, Chinese Acad emy of Sciences, Guangzhou, Guangdong); He Hongping Comparative Study on the Aggrega tion of Dif ferent Long-Chain Alkylammonia in Montmorillonite (Acta Mineralogica Sin ica, ª©ISSNªª 1000-4734, ª©CNªª52-1045/P, 23(3), 2003, p.193-198, 3 ª©illus.ªª, 23 ª©refs.ªª, with English abstract)ª¤
Keywords: montmorillonite property changing

ª¤20040192 Zhu Xuanmin (Gemmological Institute, China University of Geo sciences, Wuhan, Hubei) Study on Mineral Composition and Genesis of the Qingtian St one from Zh ejiang Province, China (Acta Petrologica et Mineralogica, ª©ISSNªª1000- 6524, ª©CNªª11-1966/P, 22(1), 2003, p.65-70, 8 ª©illus.ªª, 22 ª©refs.ªª)ª¤ Keywords: pyrophyllite jade Zhejiang Province

ª¥The author made some experiments with such means as X-ray powder diffraction analysis, infrared absorption spectral analysis, scanning electron microscopy an d differential thermal analysis in order to solve the problem of type assignment of the Qingtian stone from Zhejiang Province. The results show that the main sp ecies of Qingtian stone is of pyrophyllite type. Nevertheless, there also exist some other types, such as dickite-type, illite-type and sericite-type. This pape r has discussed mineral composition, gem features and formation mechanism of the Qingtian stone.


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PETROLOGY
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  20040193 Ding Weihua (Institute of Water Resources and Hydro-Electric Engineerin g, Xi' an University of Technology, Xi'an, Shaanxi); Wu Yanqing History and Present Si tuation of X-Ray Computerized Tomography (CT) of Rocks (Seismology and G eology, ª©ISSNªª0253-4967, ª©CNªª11-2192/P, 25(3), 2003, p.467-476, 5 ª©illus.ªª, 16 ª© refs.ªª, with English abstract)
Keywords: tomography X-ray analys is

ª¤20040194 Liu Weiguo (State Key Laboratory of Oil and Gas Reservoir Geo logy and Exploit ation, Chengdu University of Technology, Chengdu, Sichuan); Shan Yuming Study o f the Relationships Between the Dilatancy of Rocks and the Characteristics Param eters of Utrasonic Wave (Journal of Chengdu University of Technology (Sc ience & Technology Edition), ª©ISSNªª167-9727, ª©CNªª51-1634/N, 30(1), 2003, p.87-91, 3 8 ª©refs.ªª, with English abstract)ª¤
Keywords: rock mechanics ultr asonic methods

ª¤20040195 Tao Shizhen (Research Institute of Petroleum Exploration and Development of C hina, Beijing); Zhang Baomin Application of Fluid Inclusion in Oil-G as Source Trace (Acta Petrologica Sinica, ª©ISSNªª1000-0569, ª©CNªª11-1922/P, 19(2) , 2003, p.327-336, 13 ª©illus.ªª, 5 tables., 26 ª©refs.ªª, with English abstract )ª¤ Keywords: source rocks fluid inclusions Sichuan Basin China

ª¤20040196 Wei Bin (Department of Geology, Northwest University, Xi'an, Shaanxi); Wei Honghong Sediment Provenance Analysis of Yanchang Formation in Ordos Basin, Qin ghai Province, China (Journal of Northwest University, ª©ISSNªª1000-274 X, ª©CNªª61-1072/N, 33(4), 2003, p.447-450, 4 ª©illus.ªª, 2 tables, 3 ª©refs.ªª) Keywords: clastic rocks carbonate rocks Ordos Basin Shaanxi Pr ovince Inner Mongolia Gansu Province
  The sediment of Yanchang section in Ordos Basin comes from two types of paren t rock based on analysis of heavy minerals, paleocurrent and clastic particles g rading. One of the parent rock is Archaeozoic kata-playicolasegneiss and kata-sc hist in Daqing Mountain area. The second parent rock is neritopelagic detrital r ock of Sinian and Palaeozoic. The all margin of Ordos Basin in Yanchang period s upply provenance. Northern and southwestern are main province areas from early period to middle period of Yanchang Formation. Southwestern becomes main provena nce area because of its uplift in later period of Yanchang Formation.
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  20040197 Yu Qingchun (Tsukuba Software Engineering Co. Ltd., Japan) Yu zo Ohnishi Thre e-Dimensional Discrete Fracture Network Model and its Inverse Method (Ea rth Sci ence¡ª¡ªJournal of China University of Geosciences, ª©ISSNªª1000-2383, ª©CNªª41- 1233/P, 28 (5), 2003, p.522-526, 544, 4 ª©illus.ªª, 2 tables, 6 ª©refs.ªª, with English abs tract)ª¤
Keywords: ª¥crack rocks

ª¤ 20040198 Zhou Zhiguang (China University of Geosciences, Beijing); Zho u Xingguo Event s of Geochemical Characteristics for Dividing Tectonic¡ª¡ªStratigraphic Unite of P recambrian Crystal Rocks in the Yadong Area in Tibet, China (Geoscience, ª©ISSNªª10 00-8527, ª©CNªª11-2035/P, 17(3), 2003, p.237-242, 5 ª©illus.ªª, 2 tables, 7 ª©re fs.ªª, with English abstract)ª¤
Keywords: Precambrian crystalline rocks Tibet

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(1) IGNEOUSª¤PETROLOGY
ª¤ª¤20040199 Ding Daogui (Institute of Laboratory Geology of Wuxi, Jiangsu); Liu Weixin Geochemistry and Tectonic Affinities of Basic Volcanic Rocks of the Paleozoic i n Karakorum Area, NW China (Xinjiang Geology, ª©ISSNªª1000-8845, ª©CNªª6 5-1092/P, 21(1), 2003, p.96-102, 6 ª©illus.ªª, 7 ª©refs.ªª, with English abstrac t)ª¤
Keywords: ultramafics volcanic rocks back-arc basins Pamirs Tarim Basin Xinjiang

ª¤20040200 Dong Yuexia (China University of Geosciences, Wuhan, Hubei); Xia Wenchen Evolvement Sequence of Tertiary Volcanic Rocks in the Nanpu Sag, Eastern China (Petroleum Exploration and Development, ª©ISSNªª1000-0747, ª©CNªª11-2360/TE, 30( 2), 2003, p.24-26, 3 ª©illus.ªª, 4 tables, 6 ª©refs.ªª)ª¤
Keywords: volcanic rocks Huanghua Depression Hebei Province ª¥
  Deep dynamic processes and evolution of a rift basin could be determined by s tudying the magmatic evolvement within it, and establishing active sequences of volcanic rocks and to tracing their geochemical characteristics should be one of the efficient and useful tools for studying the dynamics of an extensive rift b asin. According to the comprehensive analyses of the Tertiary volcanic rocks in the Nanpu sag, rift type of evolvement could be identified, that should be a loc al rift type of evolvement sequences of decrease of lithosphere and evolvement p rocess. ª¤


ª¤20040201 Jian Ping (Institute of Geology, Chinese Academy of Geologic al Sciences, B eijing); Liu Dunyi SHRIMP Dating of Baimaª²¡¡ª©xueshanªª and Ludian Granitoid Batholit hs Northwestern Yunnan Province, and its Geological Implication (Acta G eoscien tia Sinica, ª©ISSNªª1006-3021, ª©CNªª11-3474/P, 24(4), 2003, p.337-342, 6 ª©illu s.ªª, 3 tables, 12 ª©refs.ªª)ª¤
Keywords: U-Pb dating granites Yun nan Province
  The authors studied the SHRIMP dating of Baimaxueshan and Ludian granitoid ba tholiths, and its geological implications of northwestern Yunnan Province in thi s paper. The Baimaxueshan granodiorite intruded at 239¡À6 Ma, where as the Ludian biotite monzonite granite, 214¡À6 Ma. These data pr ovide geochronological evidence for the collisional event of Jinshajiang area.

ª¤ª¤20040202 Li Fuchun (College of Resource and Environment Sciences, Nanj ing Agricultur al University, Nanjing, Jiangsu); Zhu Jinchu Experimental Evidence f or Presence of Magmatic Fe- and Li-Muscovite in the Li-F-Rich Granite (Geochimica, ª©ISSNªª037 9-1726, ª©CNªª44-1398/P, 32(1), 2003, p.75-80, 5 ª©illus.ªª, 3 tables, 18 ª©refs .ªª, with English abstract)ª¤
Keywords: granites zinnwaldite

ª¥ª¤20040203 Liu Changshi (Department of Earth Sciences, Nanjing Universit y, Nanjing, Ji angsu); Chen Xiaoming Characteristics and Origin of the Shiling Syen ite, Congª² ª©huaªª City, Guangdong Province, China (Geological Review, ª©ISSNªª0371-5736, ª©CNªª11-1952/ P, 49(1), 2003, p.28-39, 6 ª©illus.ªª, 4 tables, 1 plate, 47 ª©refs.ªª, with Eng lish abstract)ª¤
Keywords: syenites Guangdong Province

      20040204 Liu Changshi (Department of Earth Science, Nanjing Universit y, Nanjing, Ji angsu); Chen Xiaoming Origin of Nankunshan Aluminous A-Type Granite, Longkou Co unty, Guangdong Province, China (Acta Petrologica et Mineralogica, ª©IS SNªª1000-6 524, ª©CNªª11-1966/P, 22(1), 2003, p.1-10, 9 ª©illus.ªª, 4 tables, 31 ª©refs.ªª) ª¤
Keywords: A-type granites Guangdong Province
  Nankunshan aluminous A-type granite occurs in Longkou County of Guangdong Pro vince, with a outcrop area of about 200 kmª¬2. With medium-grained texture, the granite is composed of protolithionite, albite plagioclase, perthite and quartz. The rock usually is weakly peralumious and subalkaline with high alkali ration range and NK/A values. These features are obviously similar to those of aluminou s A-type granites elsewhere in the world. The discovery is important for study o n the extensional structure of late Yanshanian crust in eastern part of Nanling Mountain.
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  20040205 Liu Huimin (Department of Earth Resources and Information, un iversity of Pe troleum, Dongying, Shandong); Xie Zhonghuai Analysis on the Petroche mical Chara cteristics and Geneses of the Tertiary Igneous Rock in the Jiyang Depression, Bo haiwan Basin, China (Petroleum Geology & Experiment, ª©ISSNªª1001-6112, ª©CNªª32-1151/TE, 25(4), 2003, p.385-389, 9 ª©illus.ªª, 1 table, 12 ª©refs.ªª) ª¤
Keywords: igneous rocks Jiyang Depression Bohai Basin Shandong Province ª¥
  The petrochemicl characteristics and geneses of the Tertiary igneous rock in the Jiyang Depression, Bohaiwan Basin were discussed based on the chemical compo sition, REE and isotopic analyses of rocks. The Tertiary basalt in the Jiyang De pression can be divided into tholeiite and alkali two series. The alkali series basalt was mainly agpaitic series, and the Tertiary basaltic magmatite of this a rea whose eruptive depth was 150¡«230km was mainly continental tholeiite of cont i nental rift genesis. During the forming process of magma, mixing reaction happen ed among different source area, and melting degree decreased gradually from the Paleocene to the Oligcene, which suggested that the mantle source depth of magma increased gradually. These cognitions will of important reference significance to hydrocarbon exploration in magmatic rock.


ª¤ª¤20040206 Liu Shen (Institute of Geochemistry, Chinese Academy of Scien ces, Guiyang, Guizhou); Hu Ruizhong Geochemical Characteristics of Shoshonitic Roc ks in North ern Tibet, China (Journal of Mineralogy and Petrology, ª©ISSNªª1001-6872 , ª©CNªª51-1143 /TD, 23(2), 2003, p.66-71, 10 ª©illus.ªª, 1 table, 19 ª©refs.ªª, with English ab stract)ª¤
Keywords: volcanic rocks Tibet ª¥
ª¤ 20040207 Liu Shen (Institute of Geochemistry, Chinese Academy of Scien ces, Guiyang, Guizhou); Hu Ruizhong Geochemical Characteristics and Petrogenesis o f the Post- Collision Ultrapotassium Volcanic Rocks in Qiangtang Rock Zone, Xinjiang, China (Geotectonica et Metallogenia, ª©ISSNªª1001-1552, ª©CNªª43-1119/P, 27(2), 2003, p.167-175, 7 ª©illus.ªª, 3 tables, 27 ª©refs.ªª, with English abstract)ª¤
Keywords: volcanic rocks Tibet


ª¤20040208 Liu Wanzhu (College of Earth Sciences, Jilin University, Chan gchun, Jilin); Wang Pujun Characteristics of Deep Volcanic Reservoirs in Northern Songliao Ba sin, Liaoning Province, China (Oil & Gas Geology, ª©ISSNªª0253-9985, ª©C Nªª11-4820/TE, 24(1), 2003, p.28-31, 1 ª©illus.ªª, 2 tables, 6 ª©refs.ªª, with English abstract )ª¤
Keywords: crystalline reservoirs Songliao Plain China

ª¥ª¤20040209 Liu Xianfan (Chengdu University of Technology, Chengdu, Sichu an); Liu Jiadu o Study of Elements Geochemistry Characteristics for Ultramafic Deep Xenoliths in Alkali-Rich Porphyry (Journal of Mineralogy and Petrology, ª©ISSNªª10 01-6872, ª©CNªª 51-1143/TD, 23(3), 2003, p.39-43, 2 ª©illus.ªª, 3 tables, 17 ª©refs.ªª, with Eng lish abstract)ª¤
Keywords: porphyry rock inclusions geochemistry o f elements Yunnan Province


ª¤20040210 Liu Xiaochun (Institute of Geomechanics, Chinese Academy of G eological Scie nces, Beijing); Wang Ping'an Characteristics, Crystallization Condit ions and Em placement Depths of Quartz Monzonites from Dashui Area, Gansu Province, China (Journal of Geomechanics, ª©ISSNªª1006-6616, ª©CNªª11-3672/P, 9(1), 2003, p.62-6 9, 2 ª©illus.ªª, 3 tables, 3 ª©refs.ªª)ª¤
Keywords: monzonites gold deposits Gansu Province ª¥
  Study of petrology of quartz monzonites from Dashui area suggests that the Zh onggezhala, Zhongqu and Ge'erkuohe bodies are derived from a comagmatic region. Although their crystallization temperature of about 700 ¡æ¡«800 ¡æ is ex actly alike, the emplacement depth among them is very different, from 20 km¡«22 km of Zhonggezhala through 16 km of Zhongqu to 8 km¡«11 km of Ge'erkuohe towards the east. Moreover, the later two bodies show a signature of subvolcanic rock. This implies that hypabyssal magma is beneficial to the gold mineralization in t he Dashui area. This is why the large-scale gold deposit was defined in the vici nity of Ge'erkuohe and Zhongqu bodies, but only ore spot was found nearby Zhongg ezhala body.


ª¥ª¤20040211 Luo Zhaohua (China University of Geosciences, Beijing); Mo Xu anxue Ages of Taxkorgan Alkaline Intrusive Complex and heir Geological Implications ( Xinjian g Geology, ª©ISSNªª1000-8845, ª©CNªª65-1092/P, 21(1), 2003, 46-50, 5 ª©illus.ªª, 8 ª©refs.ªª, with English abstract)ª¤
Keywords: alkali rocks Xinjiangª¥

ª¤20040212 Qiu Ruizhao (China University of Geosciences, Beijing); Deng Jinfu Nd Isot opic Characteristics and Genesis of ª©Xianghualingªª 430 Granitic Body, Hunan Pr ovin ce, China (Acta Petrologica et Mineralogica, ª©ISSNªª1000-6524, ª©CNªª1 1-1966/P, 22(1), 2003, p.41-46, 3 ª©illus.ªª, 1 table, 36 ª©refs.ªª)ª¤ Keywords: granites neodymium isotopes Hunan Province
  Nd isotopic characteristics of rocks suggest that the granite resulted from t he mixing of the crust material with the mantle material, and that the mantle ma terial derived from the deep source got into and was distributed unevenly in the granite body. The mantle material might have mainly taken the form of mantle fl uid to join the process of granitic evolution. Under the Mesozoic background of lithosphere thinning in East China, the mantle fluid underplating induced the re melting of Meosoproterozoic strata, forming granitic magma.


ª¤ª¤20040213 Sun Hongwei (Bureau of Geological Exploration and Mineral Dev elopment, Zala ntun, Inner Mongolia); Wang Haipo A review on Adakite (Geol ogy and Re sources, ª©ISSNªª1671-1947, ª©CNªª21-1458/P, 12(1), 2003, p.61-63, 21 ª©refs.ªª) ª¤
Keywords: volcanic rocks metallogenesisª¥
  Adakite was proposed over a decade ago. It is a kind of acid-intermediate and calc-alkaline igneous rock, with the stickup characteristics of SiOª­2 greater or equal to 56%, Alª­2Oª­3 greater or equal to 15%, relatively depletive HREE an d Y (Y less then or equal to 18¡Á10ª¬ª©-6ªª, Yb¡Ü1.9¡Á10ª¬ª©-6ªª, high Sr(>400¡Á 10ª¬ª©-6ªª), La/Yb and Sr/Y, as well as positive Sr anomaly but absent or sligh tly negative Eu anomaly. There are two types of adakites with different petrogen esis: one is formed by the melting of subducting young slab, and the other is fo rmed by the partially melting of basaltic lower crust under the continental accr etion setting. Adakites are important indicators of ore deposits.


ª¤ª¤20040214 Sun Shuqin (Three Department, Chengdu University of Technolog y, Chengdu, Si chuan); Wang Yunliang Discrimination of the Tectonic Setting of Basa lts by Th, Nb and Zr (Geological Review, ª©ISSNªª0371-5736, ª©CNªª11-1952/P, 49(1), 2003, p.40-47, 6 ª©illus.ªª, 55 ª©refs.ªª, with English abstract)ª¤
Keywords: basalts ª¥

ª¤ 20040215 Wang Jian (Guangzhou Institute of Geochemistry, Chinese Acade my of Sciences , Guangzhou, Guangdong); Li Jianping Geochemical Characteristics and Geological Implications of the Cenozoic Kamafugites from Lixian County, West Qinling, China (Acta Petrologica et Mineralogica, ª©ISSNªª1000-6524, ª©CNªª11-1966/P , 22(1), 2003, p.11-19, 4 ª©illus.ªª, 4 tables, 34 ª©refs.ªª)ª¤
Keywo rds: melilitite Qinliang Mountains China
  The Cenozoic kamafugites in Lixian County of west Qinling are poor in SiOª­2 a n d Alª­2Oª­3 but rich in MgO, CaO, TiOª­2 and Kª­2O+Naª­2O. The modal mineral ass emblage is composed mainly of olivine, clinopyroxene, nepheline/kalsilite, melilite-leucit e and Ti-phlogopite. The trace isotopic compositions of Sr, Nd and trace element characteristics of kamafugitic series show distinct geochemical features simila r to those of N-OIB and MORB as well as an EMI end member caused by metasomatism of asthenospheric fluids.


ª¤ª¤20040216 Wang Pujun (College of Earth Sciences, Jilin University, Chan gchun, Jilin); Chen Shumin Relationships Between Volcanic Facies and Volcanic Rese rvoirs in S ongliao Basin, Liaoning Province, China (Oil & Gas Geology, ª©ISSNªª0253 -9985, ª©CNªª11 -4820/TE, 24(1), 2003, p.18-23, 27, 3 ª©illus.ªª, 1 table, 13 ª©refs.ªª, with En glish abstract )ª¤
Keywords: crystalline reservoirs Songliao Plain China ª¥

ª¤20040217 Wang Yang (Guangzhou Institute of Geochemistry, Chinese Acade my of Sciences , Guangzhou, Guangdong); Deng Jinfu Geodynamic Implication of Petroc hemical Fea tures of Yanshanian Strongly Peraluminous Granitoids in Wuchuan-Sihui Fracture B elt of Guangdong Province, China (Geotectonica et Metallogenia, ª©ISSNªª 1001-1552, ª©CNªª 43-1119/P, 27(1), 2003, p.56-63, 10 ª©illus.ªª, 2 tables, 17 ª©refs.ªª, with Eng lish abstract)ª¤
Keywords: granitoid geodynamics Guangdong Province

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ª¤20040218 Wang Zhaobo (No.7 Institute of Geological Exploration of Mine ral Resource, Linyi, Shandong); Zhang Xiaomei Probing into the Characteristics and Genesis of Sub-Volcanic Rock Pipe¡ª¡ªTaking Case of Shengli No.1 Kimberlite Pipe as an Example (Contributions to Geology and Mineral Resources Research, ª©ISSNªª100 1-1412, ª©CNªª1 2-1131/P, 18(1), 2003, p.54-58, 3 ª©illus.ªª, 1 table, 17 ª©refs.ªª, with Englis h abstract)ª¤
Keywords: pipes Shandong Province ª¥

ª¤ 20040219 Wu Guang (College of Earth Sciences, Jilin University, Changc hun, Jilin); L i Zhongquan Geochemical Characteristics and Genesis of the Early Mes ozoic Volca nic Rocks in Western Liaoning Province, China (Journal of Mineralogy and Petrol ogy, ª©ISSNªª1001-6872, ª©CNªª51-1143/TD, 23(3), 2003, p.44-50, 10 ª©illus.ªª, 4 tables, 21 ª©refs.ªª, with English abstract)
Keywords: Mesozoic igneous rocks lithogeochemistry Liaoning Province ª¥

ª¤ 20040220 Xiao Long (Guangzhou Institute of Geochemistry, Chinese Acade my of Sciences , Guangzhou, Guangdong); Xu Yigang Petreogensis of the Basalts of Wo niusi Forma tion at Baoshan Area, Yunnan Province: Is It of Mantle Plume Origin? (A cta Pet rologica et Mineralogica, ª©ISSNªª1000-6524, ª©CNªª11-1966/P, 22(1), 2003, p.20- 28, 8 ª©illus.ªª, 4 tables, 32 ª©refs.ªª)ª¤
Keywords: basalts Yunna n Province
  The basalts of Woniusi Formation at Baoshan area, located in western Yunnan P rovince, are composed of low-TiOª­2 tholeiites generally similar to the low-Ti t ho leiites from Emeishan large igneous province. Geochemically it consists of three eruption cycles which can be divided into three rock units. The early-stage uni t-1 basalts are characterized by massive plagioclase-phenocryst basalts, amygdal oid basalts and basaltic tuff. The middle-stage unite-2 and the late-stage unit- 3 consist of minor olivine basalts and trachybasalt as well as diabase dykes.


ª¤ª¤20040221 Xie Yunqiu (Engineering Faculty, China University of Geoscien ces, Wuhan, Hu bei); He Shiyi Karst Dynamics Features of Stone Forest under the Bas alt Cover i n Shilin Area, Yunnan Province, China (Journal of Jilin University (Eart h Scien ce Edition), ª©ISSNªª1671-5888, ª©CNªª22-1343/P, 33(3), 2003, p.340-343, 359, 4 ª©illus.ªª, 4 tables, 5 ª©refs.ªª, with English abstract)ª¤
Keywords: karst Yunnan Province

ª¥ª¤20040222 Xu Yigang (Guangzhou Institute of Geochemistry, Chinese Acade my of Sciences , Guangzhou, Guangdong); Huang Xiaolong ¡°Reactive¡± Harzburgite Xen oliths from H uinan, Jilin Province and their Implications for Deep Dynamic Processes (Acta P etrologica Sinica, ª©ISSNªª1000-0569, ª©CNªª11-1922/P, 19(1), 2003, p.19-26, 6 ª©illus.ªª, 1 table, 32 ª©refs.ªª, with English abstract)ª¤
Keywords: harzdurgite rock inclusions Jilin Province ª¥

ª¤ 20040223 Zhang Qi (Institute of Geology and Geophysics, Chinese Academ y of Sciences, Beijing); Wang Yan On the Relationships Between Adakite and its Tec tonic Setting (Geotectonica et Metallogenia, ª©ISSNªª1001-1552, ª©CNªª43-1119/P, 27 (2), 2003, p.101-108, 1 ª©illus.ªª, 1 table, 49 ª©refs.ªª, with English abstract )ª¤
Keywords: Eclogite Dabie Mountains China

ª¤ 20040224 Zhang Qi (Institute of Geology and Geophysics, Chinese Academ y of Sciences, Beijing); Zhou Guoqing Distribution of Time and Space of Chinese Op hiolites an d their Tectonic Settings (Acta Petrologica Sinica, ª©ISSNªª1000-0569, ª©CNªª11-19 22/P, 19(1), 2003, p.1-8, 3 ª©illus.ªª, 35 ª©refs.ªª, with English abstract)ª¤
Keywords: ophiolite North China Platform Tarim Basin Yangtze Platf orm China ª¤


  20040225 Zhang Yong (School of Earth and Space Science, Peking University, Beiji ng); Chen Bin Geochemistry and Origin of Late Mesozoic Lamprophyre Dykes in Taihang Mountains, North China (Acta Petrologica et Mineralogica, ª©ISSNªª1000 -6524, ª©CNªª11-1966/P, 22(1), 2003, p.29-33, 5 ª©illus.ªª, 1 table, 26 ª©refs. ªª)ª¤
Keywords: lamprophyres Taihang Mountains China
  Numerous lamprophyre dykes occur and cut through the Late Mesozoic granitic c omplexes in Taihang Mountains, North China Craton. These dykes are highly enrich ed in LIL elements such as Rb, Sr, Ba and K as well as light REE. The highly fra ctioned REE patterns and the regular variation in chemical and Nd-Sr isotope com position show that these lamprophyres were produced from the fractionation of th e parent magma, and the ascending magma was contaminated by the lower crust. The mantle was enriched in the Middle Proterozoic, during when volatile-rich and lo w-density melts were released by asthenosphere interacting with the above lithos phere.


ª¤ª¤20040226 Zheng Jianping (Faculty of Earth Sciences, China University o f Geosciences, Wuhan, Hubei); Lu Fengxiang Mantle Replacement: Evidence from Compa rison in Tr ace Elements Between Peridotite and Diopside from Refractory and Fertile Mantle, North China (Earth Science¡ª¡ªJournal of China University of Geoscience s, ª©ISSNªª10 00-2383, ª©CNªª42-1233/P, 28(3), 2003, p.235-240, 2 ª©illus.ªª, 2 tables, 23 ª©r efs.ªª, with English abstract)ª¤
Keywords: lithosphere peridotites North China Platform

ª¤ 20040227 Zhou Haimin (China University of Geosciences, Wuhan, Hubei); Ma Qian Chara cteristics of Pyrolith Reservoirs in Beipu Area, Nanpu Sag, Hebei Province, China (Oil & Gas Geology, ª©ISSNªª0253-9985, ª©CNªª11-4820/TE, 24(1), 2003, p.36-38, 2 ª©illus.ªª, 2 ª©refs.ªª, with English abstract)ª¤
Keywords : crystalline reservoirs Huanghua Depression Hebei Province

ª¤ 20040228 Zhou Hui (Department of Geology, Beijing); Yuan Chao Material and Heat Sou rces of the Early Paleozoic Magmatic Rocks in Kuda, Western Kunlun, Xinjiang, China (Xinjiang Geology, ª©ISSNªª1000-8845, ª©CNªª65-1092/P, 21(1), 2003, p.65-68, 1 ª©illus.ªª, 1 table, 17 ª©refs.ªª, with English abstract)ª¤ Keywords: igneous rocks Kunlun Mountains Xinjiang

ª¤ 20040229 Zhou Jincheng (Department of Earth Sciences, Nanjing Universi ty, Nanjing, J iangsu); Wang Xiaolei Lithogeochemistry of Meso- and Neoproterozoic Mafic-Ultra mafic Rocks from Northern Guangxi Province, China (Acta Petrologica Sini ca, ª©ISSNªª 1000-0569, ª©CNªª11-1922/P, 19(1), 2003, p.9-18, 11 ª©illus.ªª, 2 tables, 36 ª©r efs.ªª, with English abstract)ª¤
Keywords: ultramafics Guangxi Province ª¤

(2) METAMORPHICª¤PETROLOGY
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  20040230 Cheng Hao (School of Earth Space Sciences, University of Science and Technology of China, Hefei, Anhui); Chen Daogong Optimized Geospeedo metry: Evid ence for Slow Cooling of the Huangtuling Granulite, Northern Dabie Mountains, China (Geochimica, ª©ISSNªª0379-1726, ª©CNªª44-1398/P, 32(2), 2003, p.167- 172, 4 ª©illus.ªª, 1 table, 42 ª©refs.ªª, with English abstract)ª¤
Keywords: orogenic belts granulites Dabie Mountains Chinaª¤

   20040231 Guo Jinjing (Department of Civil Engineering, Tianjin Institu te of Urban Co nstruction, Tianjin); Li Huaikun Brief Review of the Study of Qinlin g Orogenic Belt, China (Geological Survey and Research, ª©ISSNªª1672-4135, ª©CNªª12 -1353/P, 26(2), 2003, p.95-102, 2 tables, 31 ª©refs.ªª, with English abstract)ª¤ Keywords: Precambrian Qinling Mountains Chinaª¤
  

  20040232 Guo Lequn (Hunan Institute of Geology Survey, Xiangtan, Hunan); Tang Xi aosh an Northeastern Hunan Province the Lianyunshan Complex Primary Resea rch (Hunan Geology, ª©ISSNªª1001-4756, ª©CNªª43-1147/P, 22(2), 2003, p.87-95, 7 ª©illus.ªª , 3 tables, 3 ª©refs.ªª)ª¤
Keywords: metamorphic rocks Hunan Provinceª¥
  The Lianyunshan complex is metamorphic rock formed for regional metamorphism of high greenschist-amphibolite facies and matization and contact thermal metamo rphism minerals of metamorphic consist of St+Sill+Cr+Hb+Ab+Bi+Pl+Qz. Sm-Nd whole rock isochrom is 1 960¡À50 Ma and 1 905¡À25 Ma. The p rotoliths and the geochemistry characteristics show is formed of continent margi n arc and represent the paleoproterozoic crystalline basement of the southeast Y angtze.
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ª¤20040233 Jia Wanglu (Faculty of Earth Sciences, China University of Ge osciences, Wuh an, Hubei); Gao Shan Evidence of Partial Melting of Eclogites from D abie-Sulu U ltrahigh-Pressure Metamorphic Belt: Trace Elements and Pb Isotope (Earth Scienc e¡ª¡ªJournal of China University of Geosciences, ª©ISSNªª1000-2383, ª©CNªª42-123 3/P, 28( 2), 2003, p.121-128, 5 ª©illus.ªª, 4 tables, 20 ª©refs.ªª, with English abstract )ª¤
Keywords: Eclogite Dabir Mountains China ª¥

ª¤ 20040234 Li Sanzhong (College of Marine Geoscience, Ocean University o f China, Qingd ao, Shandong); Lai Shaocong Metamorphic Dynamics of the Mian-Lue Sut ure Zone of Qinling Orogenic Belt and the Southern Qinling Block, China (Chinese Jo urnal o f Geology, ª©ISSNªª0563-5020, ª©CNªª11-1937/P, 38(2), 2003, p.137-154, 2 ª©illus .ªª, 2 plates, 83 ª©refs.ªª, with English abstract)ª¤
Keywords: meta morphic belts P-T-t trace Qinling Mountains China

ª¤ 20040235 Li Weidong (China University of Geosciences, Wuhan, Hubei); P en Xiangping Petrographic Geochemical Features and their Tectonic Significance of Ophiolite o f Changliugou of Muzitage in East Kunlun, Xinjiang, China (Xinjiang Geol ogy, ª©ISSNªª 1000-8845, ª©CNªª65-1092/P, 21(3), 2003, p.263-268, 6 ª©illus.ªª, 7 tables, 6 ª© refs.ªª, with English abstract)ª¤
Keywords: ophiolite Xinjiangª¥ª¤

   20040236 Liang Bing (Institute of Earth Science, China University of G eosciences, Wu han, Hubei); He Wenjing Regional Very Low-Grade Metamorphism of Tria ssic Xikang Group in Xiangtang Area, Northwest Sichuan Province, China (Journal of Mineral Petrology, ª©ISSNªª1001-6872, ª©CNªª51-1143/TD, 23(1), 2003, p.42-45, 2 ª©illus .ªª, 2 tables, 12 ª©refs.ªª)ª¤
Keywords: low-grade metamorphism Sic huan Province ª¥
  Regional geological research and analysis of illite crystallinity, bª­0 paramet ers indicated that Triassic Xikang Group underwent a regional very low-grade met amorphism in Xiangtang area, northwest Sichuan Province. Relationships between r egional very low-grade metamorphism and regional deformation discussed in this p aper. Regional very low-grade metamorphism results from the combination of early diagenesis-burial metamorphism and late syn-orogeny metamorphism.

ª¤20040237 Liu Xiaochun (Institute of Geomechanics, Chinese Academy of G eological Scie nces, Beijing); Zhao Yue Pan-African Granulite Facies Metamorphism i n the Grove Mountains, East Antarctica (Geological Review, ª©ISSNªª0371-5736, ª©CN ªª11-1952/P, 49( 4), 2003, p.422-431, 4 ª©illus.ªª, 4 tables, 58 ª©refs.ªª, with English abstract )
Keywords: granulites metamorphism Antarctica ª¥

ª¤ 20040238 Liu Yongsheng (Faculty of Earth Sciences, China University of Geosciences, Wuhan, Hubei); Hu Shenghong Accurate Analysis of Zr, Hf, Nb and Ta i n High-Grad e Metamorphic Rocks with ICP-MS (Earth Science¡ª¡ªJournal of China Unive rsity of Geosciences, ª©ISSNªª1671-2383, ª©CNªª42-1233/P, 28(2), 2003, p.151-156, 2 ª©ill us.ªª, 6 tables, 11 ª©refs.ªª, with English abstract)ª¤ Keywords: me tamorphic rocks inductively coupled plasma mass spectrometry ª¤ 20040239 Lu Baoqi (Material School of Shanghai University, Shanghai); Wang Ciyin Study on the Designation of the Metamorphic Belts and their Genesis in L¨¹liang G r oups in Luofan Districts Shanxi Province, China[WT][ST] (Acta Geoscientia Sinic a, ª©ISSNªª 1006-3021, ª©CNªª11-3474/P, 24(4), 2003, p.325-329, 2 ª©illus.ªª, 3 tables, 17 ª©refs.ªª)ª¤
Keywords: metamorphic facies Shanxi Province
  The original layers of metamorphic rocks of L¨¹liang Group in Loufan district Shanxi Province consist of the muddy sedimentary and igneous rocks, which had un dergone the two different metamorphism, namely: the early L¨¹liang metamorphisms and the lake fault-type ductile shear deformation metamorphisms. The former caus ed the northeast layer's occurrence, while the latter had the northeast layer's occurrence turned to the nearly north-south and overlapped on the former and clo sely linked to the formation of metamorphic belts.
ª¤

ª¤20040240 Lu Songnian (Tianjin Institute of Geology and Mineral Resourc es, Tianjin); Li Huaikun Preliminary Study of Giant-Crystal Garnet-Gedrite Rocks i n Hengshan Mountain, Shanxi Province, China (Geological Survey and Research, ª©ISSN ªª1672-4135 , ª©CNªª12-1353/P, 26(1), 2003, p.15-20, 26, 2 ª©illus.ªª, 3 tables, 10 ª©refs. ªª, with English abstract)ª¤
Keywords: metaigneous rocks Shanxi Province ª¥

ª¤20040241 Ou Xingong (Faculty of Earth Sciences, China University of Ge osciences, Wuh an, Hubei); Jin Zhenmin Thermal Conductivity of Donghai UHP Eclogite and its Si gnificance for Studying Continental Scientific Drilling (Earth Science¡ª ¡ªJournal of China University of Geosciences, ª©ISSNªª1000-2383, ª©CNªª42-1233/P, 28(2), 2003, p.129-135, 6 ª©illus.ªª, 3 tables, 22 ª©refs.ªª, with English abstract)ª¤
Keywords: ec logite Continental Scientific Drilling Program Jiangsu Province East China Sea ª¤

ª¤20040242 Qiu Haijun (Faculty of Earth Sciences, Jilin University, Chan gchun, Jilin); Xu Zhiqin The Discovery of Glaucophane Greenschist Facies Rock Mass in Lianyun gang, Northern Jiangsu Province, China (Acta Petrologica et Mineralogic a, ª©ISSNªª 1000-6524, ª©CNªª11-1966/P, 22(1), 2003, p.34-40, 3 ª©illus.ªª, 2 tables, 39 ª©r efs.ªª)
Keywords: blueschist greenschist Jiangsu Province
ª¤The Sulu high-pressure (HP) metamorphic belt lies on the southeastern margin of the Sulu ultrahigh-pressure (UHP) metamorphic belt in northern Jiangsu Provin ce. Its outcrops consist mainly of greenschist-facies rocks of the Meso- to Neop roterozoic Yuntai Group-complex. Nevertheless, typical blueschist was only found in the drilling cores from Yangji Town of Guanyun County in northern Jiangsu Pr ovince. The glaucophane greenschist facies rocks discovered in such places of Li anyungang area as Hongshizui, Dongxiliandao and Xieqigou consist of winchite, ba rroisite, actinolite, albite, phengite, sphene, aragonite, etc.
ª¤ª¤

ª¤20040243 Suo Shutian (Faculty of Earth Sciences and Mineral Resources, China Univers ity of Geosciences, Beijing); Zhong Zengqiu Massive Eclogites and th eir Tectoni c Significance in Dabie-Sulu UHP Metamorphic Belt, East-Central China (E arth Sc ience¡ª¡ªJournal of China University of Geosciences, ª©ISSNªª1000-2383, ª©CNªª42 -1 233/P, 28(2), 2003, p.111-120, 9 ª©illus.ªª, 54 ª©refs.ªª, with English abstract )ª¤
Keywords: Eclogite ultra-high pressure metamorphism Dabie Moun tains China ª¥

ª¤20040244 Tao Jixiong (Geological Survey of Inner Mongolia, Hohhot, Inn er Mongolia) Characteristics of Neoarchean Metamorphic Intrusive and the Relationships with t he Mineralization of Gold in Guyang Region, Inner Mongolia, China (Geolo gical S urvey and Research, ª©ISSNªª1672-4135, ª©CNªª12-1353/P, 26(1), 2003, p.21-26, 4 ª©illus.ªª, 3 tables, 6 ª©refs.ªª, with English abstract)
Keywords: metavolcanic rocks Inner Mongolia

ª¤20040245 Wang Linsen (Faculty of Earth Sciences, China University of G eosciences, Wu han, Hubei); Zhang Li Pb Isotopic Analysis Technique of Eclogite fro m Dabie-Sul u Orogenic Belt, China (Earth Science¡ª¡ªJournal of China University of Geoscienc es, ª©ISSNªª1671-2383, ª©CNªª42-1233/P, 28(2), 2003, p.136-142, 3 tables, 13 ª©r efs.ªª)
Keywords: Eclogite lead-zinc isotopes Dabie Mountains China
ª¤Pb isotopes have been comprehensively applied to isotopic geocheronology, geochemical tracing and division of tectonic zones. Due to the difficulty for calib ration of Pb isotopic fractionation in thermal ionization mass spectrometry (TIM S) analysis, the accurate determination of Pb isotopic ratios, especially for lo w-Pb samples, is generally difficult. This paper reports the preparation of samp les with low-Pb contents, process of TIMS analysis and confect of emission reage nt for accurate Pb isotope analysis.
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ª¤20040246 Wang Lu (Graduate School, China University of Geosciences, Wu han, Hubei); J in Zhenmin Raman Spectrum Study on Quartz Exsolution in Omphacite f rom Eclogit e and its Tectonic Significances (Earth Science¡ª¡ªJournal of China Univ ersity of Geosciences, ª©ISSNªª1671-2383, ª©CNªª42-1233/P, 28(2), 2003, p.143-150, 6 ª©il lus.ªª, 34 ª©refs.ªª, with English abstract)ª¤
Keywords: Eclogite coesite

ª¤20040247 Xu Qidong (Faculty of Earth Resources, China University of Ge osciences, Wuh an, Hubei); Zhong Zengqiu Fluid Inclusion Associations and their Dev elopment in the Dabie UHP Zone, China (Acta Petrologica et Mineralogica, ª©ISSNªª1 000-6524, ª©CNªª11-1966/P, 22(1), 2003, p.47-54, 6 ª©illus.ªª, 37 ª©refs.ªª)ª¤ Keywords: me tamorphic belt of high pressure fluid inclusions Dabie Mountains China ª¥
ª¤The fluid inclusions in several types of rocks in the Dabie UHP zone were sys tematically investigated in the aspects of petrography and temperature of phase change. The fluid inclusion associations related to distinct fluid-related event s were often superimposed on the rocks in UHP and retrograde metamorphism, and h ence the geological explanation for chemical and isotopic composition of fluid i nclusions based on bulk inclusion analysis is subject to some risk.
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ª¤20040248 Zhang Haixiang (Guangzhou Institute of Geochemistry, Chinese Academy of Sci ences, Guangzhou, Guangdong); Zhang Boyou Study on the Metamorphism and Metamor phic Age from Xingzi Group, Lushan Mountains, Jiangxi Province, China (J ournal of Mineralogy and Petrology, ª©ISSNªª1001-6872, ª©CNªª51-1143/TD, 23(2), 2003, p .32-36, 4 tables, 16 ª©refs.ªª, with English abstract)ª¤
Keywords: m etamorphic rocks Jiangxi Province ª¥

ª¤ 20040249 Zhang Xiping (Beijing Institute of Geology and Mineral Resour ces, Beijing); Wan Yusheng Geology and Petrography of the Pingyang Gneissic Trondh jemite, ª©Fup ingªª, Hebei Province, China (Geology in China, ª©ISSNªª1000-3657, ª©CN ªª11-1167/P, 30(1) , 2003, p.61-72, 4 ª©illus.ªª, 1 plate, 31 ª©refs.ªª, with English abstract)ª¤
Keywords: trondhjemite Hebei Province ª¤
ª¤20040250 Zhou Yongsheng (Institute of Geology and Tectonophysics Laboratory, Chi nese Academy of Sciences, Beijing); He Changrong Melt Characteristics of Partial Me lted Gabbro under Plastic Deformation Condition (Chinese Journal of Geop hysics, ª©ISSNªª0001-5733, ª©CNªª11-2074/P, 46(4), 2003, p.482-487, 3 ª©illus.ªª, 2 tab les, 17 ª©refs.ªª, with English abstract)
Keywords: gabbros triax ial tests ª¥

ª¤

(3) SEDIMENTARYª¤PETROLOGY
ª¤ª¤
ª¤20040251 Chen Shiyue (University of Petroleum, Dongying, Shandong); Yan Jihua Evol ution of Sedimentary Facies of the Paleogene in Binnan-Lijin Areas, Dongying Sag , Shandong Province, China (Petroleum Exploration and Development, ª©IS SNªª1000-0747, ª©CNªª11-2360/P, 30(3), 2003, p.36-38, 5 ª©illus.ªª, 5 ª©refs.ªª)
Keywords: sedimentary facies Dongying Depression Shandong Province
ª¤There were many sedimentary facies in Binnan-Lijin areas of the Dongying sag in the Paleogene, such as fan delta, inshore submerged fan, shallow lake, semi-d eep lake and deep lake. From bottom to upper sections, the sedimentary facies ve rtically evolved in such order: fan delta-semi-deep lake, deep-lake-shallow lake . It is suggested that the main periods of supplying sediments are the Sha-4 and the later Sha-3 sedimentation episodes based on lithologic statistics in over e ighty wells. Except for Sha-4, in the other periods of the Paleogene, the ª©Chen jiazhuangªª salient provided more sediments than the Binxian salient.
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ª¤20040252 Dong Chunmei (Graduate School, Research Institute of Geology and Geophysic s, Chinese Academy of Sciences, Beijing); Song Chungang Study on the Sedimentar y Microfacies of the Sha-3 Member in Bonan Oilfield, China (Petroleum G eology & Experiment, ª©ISSNªª1001-6112, ª©CNªª32-1151/TE, 25(4), 2003, p.375-380, 4 ª©i llus.ªª, 2 tables, 5 ª©refs.ªª)
Keywords: sedimentary microfacies lithologic traps Bohai Basin China ª¥
ª¤Aimed at high exploration degree of the Sha-3 member in Bonan oilfield, the B onan sag of the middle Zhanhua Depression, the sedimentary microfacies were stud ied on the base of high-resolution sequence stratigraphical research, and sedime ntary lobes were found as important targets for hydrocarbon exploration. During the Sha-3 period of the Bonan sag, the essential sources from the Gudao convex a nd the secondary sources from the Luojia Nose formed the deep-lake turbidite-fan sedimentary system, including endofan, mesofan and exofan three subfacies and e ndofan feeding channel, endofan terrace, endofan natural levee, mesofan braided channel, mesofan lobe and exofan sheet and six microfacies.


ª¤ª¤20040253 Du Hongyu (Research Institute of Exploration and Development, Turpan-Hami O ilfield Company, PetroChina, Hami, Xinjiang); Wang Hongyan Geochemic al Characte ristics of Lucaogou Source Rock in Malang Sag, Santanghu Basin, Xinjiang, China (Xinjiang Petroleum Geology, ª©ISSNªª1001-3873, ª©CNªª65-1107/TE, 24(4), 2003, p.302-305, 5 ª©illus.ªª, 1 table, 4 ª©refs.ªª)ª¤
Keywords: source r ocks Xinjiang
ª¤In this paper, the authors studied the Lucaogou source rock in Malang sag, Sa ntanghu Basin. The result shows that: 1) primary origin of asphaltene assumes pr edominant distribution in which organic matter could mainly come from bio-degrad ation of thallophyte; 2) the biomarker composition in soluble organic matter app ears to be of general feature of mixed sources from both terrigenous higher plan t and microorganism, with abundant hydrogen composition; and 3) the sample of so urce rock reflects the characteristics of macroscopic pyrolysis with higher oil threshold temperature and narrower major hydrocarbon generation zone, similar to the hydrocarbon generation pattern of Type I kerogen.
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ª¤20040254 Duan Jiye (College of Earth Science, Jilin University, Changc hun, Jilin); L iu Pengju Abysmal and Sub-Abysmal Deposit of Mesoproterozoic in Yans han Aulocog en, North China (Journal of Jilin University (Earth Science Edition), ª© ISSNªª1671- 5888, ª©CNªª22-1343/P, 33(1), 2003, p.7-14, 1 ª©illus.ªª, 2 plates, 1 table, 6 ª©refs.ªª, with English abstract)ª¤
Keywords: deep-water environment sedimentary sequence Yanshan Mountains China ª¥

ª¤ 20040255 Fang Aimin (Institute of Geology and Geophysics, Chinese Acad emy of Science s, Beijing); Hou Quanlin Turbiditic Facies and their Characteristics of Abyssal Turbidities in the Kuda Melange Belt in West Kunlun, Xinjiang, China (C hinese Journal of Geology, ª©ISSNªª0563-5020, ª©CNªª11-1937/P, 38(1), 2003, p.1-12, 2 ª©illus.ªª, 2 plates, 1 table, 26 ª©refs.ªª, with English abstract)ª¤
Keywords: turbidite deep-sea environment Kunlun Mountains ª¥

ª¤ 20040256 Feng Xingqiang (Geological and Geophysical Institute, Chinese Academy of Sc iences, Beijing); Yang Changchun Study of Sedimentary Facies of Can gfanggou Gr oup in Bajiahai-Wucaiwan Area of Eastern Junggar Basin, Xinjiang, China (Xinji ang Petroleum Geology, ª©ISSNªª1001-3873, ª©CNªª65-1107/TE, 24(1), 2003, p.41-43 , 4 ª©illus.ªª, 4 ª©refs.ªª)ª¤
Keywords: Triassicsedimentary facies Junggar Basin Xinjiang ª¥
ª¤Six types of sedimentary facies are identified according to available data fr om Cangfanggou Group in Baijiahai-Wucaiwan area of Eastern Junggar Basin, in whi ch each lithology feature, sedimentary structure and vertical sequence are analy zed in detail. Furthermore, planar distribution of the facies are described. Fin ally, the sedimentary model has been developed, which offers a reliable basis fo r further exploration of its favorable petroliferous facies in this area.

ª¤ª¤20040257 Fu Suotang (State Key Laboratory of Oil and Gas Reservoir Geo logy and Explo ration, Chengdu University of Technology, Chengdu, Sichuan); Tian Jingchun The Delta Depositional System Distribution of Late Paleozoic Era in Ordos Basin, China (Journal of Chengdu University of Technology (Science & Technology Ed ition), ª©ISSNªª1671-9727, ª©CNªª51-1634/N, 30(3), 2003, p.236-241, 7 ª©illus.ªª, 1 tab le, 9 ª©refs.ªª, with English abstract)ª¤
Keywords: deltaic anvironm ent depositional system Ordos Basin China

ª¤ 20040258 Gong Yiming (China University of Geosciences, Wuhan, Hubei); Xu Ran Ripple Marks with Bifurcation from the Calcareous Turbidite Sequence of Upper Devonian in Guangxi Province, South China (Geological Review, ª©ISSNªª0371-5736, ª©CNªª11-1952/ P, 49(4), 2003, p.379-382, 2 ª©illus.ªª, 44 ª©refs.ªª, with English abstract)ª¤
Keywords: turbidite ripple marks Guangxi Province ª¤

ª¤20040259 Gu Yunfei (Research Institute of Geology and Geophysics, Chinese Acade my o f Sciences, Beijing); Ma Mingfu Lithofacies Paleogeography of the C retaceous i n the Junggar Basin, Xinjiang, China (Petroleum Geology & Experiment, ª©ISSNªª1001 -6112, ª©CNªª32-1151/TE, 25(4), 2003, p.337-342, 347, 4 ª©illus.ªª, 2 tables, 8 ª©refs.ªª)ª¤
Keywords: lithofacies palaeogeography Junggar Basin Xinjiang ª¥
ª¤The lithofacies paleogeographical characteristics of the Cretaceous in the Ju nggar Basin were analysed based on the outcrop, drilling, logging and seismic da ta. The basin developed alluvial fan, braided stream, alluvial plain, delta, sho re shallow lake and semideep lake sedimentary facies. Lithologically, the alluvi al fan was dominated by sand conglomerate, the braided stream by gravelly sandst one and moderatefine sandstone, the delta by microsandstone and siltstone, and t he alluvial plain, the shore shallow lake and the semideep lake by mudstone. The delta sandbodies of the Qingshuihe Group and the Hutubihe Group were the favora ble reservoirs and exploration targets of the Cretaceous in the basin.
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ª¤20040260 Huang Sijing (State Key Laboratory of Oil and Gas Reservoir G eology and Exp loitation, Chengdu University of Technology, Chengdu, Sichuan); Shi He Diagenet ic Alteration of Earlier Paleozoic Marine Carbonate and Preservation for the Inf ormation of Sea Water (Journal of Chengdu University of Technology (Scie nce & T echnology Edition), ª©ISSNªª1671-9727, ª©CNªª51-1634/N, 30(1), 2003, p.9-18, 2 ª©illus.ªª, 1 table, 33 ª©refs.ªª, with English abstract)ª¤ Keywords: carbonate rocks

ª¤20040261 Jiang Xinsheng (Institute of Sedimentary Geology, Chengdu Uni versity of Tec hnology, Chengdu, Sichuan); Zhu Tongxing Discovery of the Late Trias sic Coastal Aeolian Dune in South Tibet Tethys and its Significance (Journal of Che ngdu Un iversity of Technology (Science & Technology Edition), ª©ISSNªª1671-9727, ª©CNªª 51- 1634/N, 30(5), 2003, p.447-452, 5 ª©illus.ªª, 15 ª©refs.ªª, with English abstrac t)
Keywords: Upper Triassic Tethys dunes

ª¤ 20040262 Lei Kaiqiang (Chengdu University of Technology, Chengdu, Sich uan); Kong Fan zheng Diagenesis of Sandstone in the Upper Paleozoic in Tabamiao Are a of Ordos Basin and Reconstruction of the Storage Space of Sandstone (Journal of M ineralo gy and Petrology, ª©ISSNªª1001-6872, ª©CNªª51-1143/TD, 23(3), 2003, p.92-96, 2 ª©illus.ªª, 3 tables, 7 ª©refs.ªª, with English abstract)
Keywords: Upper Palaeozoic sandstone Ordos Basin ª¥

ª¤ 20040263 Li Yan (Information Center of Geological Material Objects, M LR, Sanhe, Heb ei) Fan-Deltaic Depositional Systems of the Xiguayuan Formation in Luanping Ba sin, Hebei Province, China (Acta Geoscientia Sinica, ª©ISSNªª1006-3021, ª©CNªª11-3474/P, 24(4), 2003, p.353-356, 4 ª©illus.ªª, 1 table, 8 ª©refs.ªª) Keywords: depositional system fan deltas Hebei Province
ª¥In this paper, the author studies the fan-deltaic depositional systems of the Xiguayuan Formation in Luanping Basin. Lower Cretaceous Xiguayuan Formation in southwestern Luanping Basin is characterized by fan-deltaic depositional success ions. The depositional system of Luanping fan-delta can be further divided into 3 sedimentary associations and 17 genetic units. Depositional microfacies of all genetic units are described in this paper.

ª¤20040264 Liu Jun (Jianghan Petroleum Institute, Jingzhou, Hubei); Li Shaohua Resea rch on Sedimentary Microfacies Using Sequential Indicator Simulation (P etroleu m Geology & Oilfield Development in Daqing, ª©ISSNªª1000-3754, ª©CNªª23-1286/TQ, 22(2), 2003, p.11-12, 46, 2 ª©illus.ªª, 1 table, 2 ª©refs.ªª)ª¤
Keywords: numerical simulation sedimentary microfacies ª¥
ª¤It is difficult to determine and classify the boundary of sedimentary microfa cies in the study of reservoir sedimentation. This paper applies sequential indi cator simulation to model the spatial distribution of sedimentary microfacies of Chang4+5ª­2 in P oilfield. The result shows that this approach not only demon st rates the variation of microfacies, but also overcomes the uncertainty of the mo dels due to the lack of data. It gives a solid geological foundation for forecas ting reservoir parameters in the further study.

ª¤20040265 Lu Hongyou (Guangzhou Institute of Geochemistry, Chinese Acad emy of Science s, Guangzhou, Guangdong); Cao Yingchang The Basic Equation of Sedime ntation and its Application in Rift Lake Basin (Petroleum Exploration and Developm ent, ª©ISSNªª 1000-0747, ª©CNªª11-2360/P, 30(3), 2003, p.19-22, 4 ª©illus.ªª, 16 ª©refs.ªª)
Keywords: fault-downwarping basins sedimentation ª¥
ª¤Sedimentation of lake basin is controlled by the following factors: climate, structure, sediment supply, sea level change and so on. Combined with the discus sion of the sedimentary basic equation and the signification of every parameter, the forming mechanism of sequence boundary and the principles of lake regressio n and lake transgrassion were interpreted. The formation of the sequence boundar y was controlled by climate changing, structural lifting and differential vibrat ory movement which are the three forming mechanisms of the sequence boundary.


ª¤ª¤20040266 Ma Yingjian (Department of Geoscience, Nanjing University, Na njing, Jiangsu ); Wang Changsheng Fine Sedimentary Facies Research of Oil Reservoir in Pu-I Fo rmation, Pubei Oilfield, Songliao Basin, Liaoning Province, China (Jour nal of Daqing Petroleum Institute, ª©ISSNªª1000-1891, ª©CNªª23-1297/TE, 27(2), 2003, p. 8-12, 3 ª©illus.ªª, 1 table, 5 ª©refs.ªª)ª¤
Keywords: oil reservoirs Songliao Plain China
ª¤The oil reservoir in Pu-I Formation, Pubei oilfield, Songliao Basin, has its own characteristics. In the plane, the sand developed in a small scale and was d ispersely distributed. In the long itudinal section, the thin intermediate layer with heavy mud and heavy calcium present distinct characteristics. This paper s ubdivides the oil reservoir of Pu-I Formation as 3 sandstone formations, 11 smal l layers and 26 sedimentary units. The subdivision is made by viewing the sedime ntary sand formation of stage on as the minimal units of petrofacies subdivision and comparisons, cyclic comparison and multiple stage control according to the same stage comparing principle.

ª¤20040267 Miao Jianyu (Key Laboratory of Continental Dynamics, Ministry of Education, Northwest University, Xi'an, Shaanxi); Zhu Zongqi Characteristics o f Pore Stru ctures of Paleogene-Neogene Argillaceous Rocks in the Jiyang Depression, Shandon g Province, China (Geological Review, ª©ISSNªª0371-5736, ª©CNªª11-1952/P , 49(3), 2003, p.330-336, 3 ª©illus.ªª, 1 table, 10 ª©refs.ªª, with English abstract)
Keywords: shale reservoirs porosity Jiyang Depression Shandong Province ª¥ª¤


ª¤20040268 Ouyang Rui (Science Research Institute of Exploration and Development o f Zh ongyuan Oil Field Company, Puyang, Henan); Jiao Cunli The Distributi on and Feat ures of Reef in Tazhong Area of Tarim Basin Northwest China (Petroleum Explora tion and Development, ª©ISSNªª1000-0747, ª©CNªª11-2360/TE, 30(2), 2003, p.33-36, 2 ª©illus.ªª, 2 tables, 6 ª©refs.ªª)ª¤
Keywords: reefs Tarim Basin Xinjiang
ª¤There are many kinds of reef in Tazhong area of Tarim Basin, Northwest China in age of Middle-Upper Ordovician. The main reef-building organisms are ª§Sponge s, Calathium, Stromatoporoids, Corals, Crytalgaes, Bryozoans, Blue-green algae, Ch orophyteª§ and ª§Rhodophyteª§ in Solenoporaceae. The reef can be divided into ca lcilut ite mound, framework reef and baffle reef. The analysis on the reef encountered during the drilling shows that the calcilute mound is mainly formed in continent al shelf and inner zone of the shelf margin, while framework reef and baffle ree f are mainly in the shelf and the shelf margin. And by studying the sedimentary facies and the features of seismic reflection in this area, it can be predicted that reef with the distribution shapes of belt and discontinuous belt can be fou nd in the shelf margin area of Tazhong uplift and in the middle area of northern slope of Tazhong area.
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ª¤20040269 Shan Xiuqin (Langfang Branch of RIPED of PetroChina, Langfang , Hebei); Hu G uoyi Paleocurrent Energy Study with Inclusion of Calcite Gangue for Ordovician System in Central Ordos Basin, China (Acta Petrologica Sinica, ª©ISSNªª1 000-0569, ª©CNªª 11-1922/P, 19(2), 2003, p.355-358, 3 ª©illus.ªª, 1 table, 5 ª©refs.ªª, with Engl ish abstract)
Keywords: fluid potential migration o fpetroleum O rdos Basin China

ª¤20040270 Shi Chenghua (No.1 Hydrogeological & Engineering Geological P arty of Zhanji ang, Guangdong) Rock Assemblage Features and Ore-Bearing Characteris tics of the Tianyang Formation in the Leizhou Peninsula, Guangdong Province, China (Guangd ong Geology, ª©ISSNªª1001-8670, ª©CNªª44-1201/P, 18(2), 2003, p.1-8, 2 ª©illus. ªª, 6 tables, 1 ref., with English abstract)
Keywords: Pleistocene lithostratigraphy Guangdong Province

ª¤ 20040271 Shou Jianfeng (Hangzhou Institute of Petroleum Geology, RIPE D, PetroChina, Hangzhou, Zhejiang); Shao Wenbin Lithological Types and Distributi on Features of Tertiary Algal-Limestone in Chaixi Area, Qaidam Basin, Qinghai Province, China (Petroleum Exploration and Development, ª©ISSNªª1000-0747, ª©CNªª11- 2360/TE, 30(4), 2003, p.37-39, 3 ª©illus.ªª, 2 tables, 6 ª©refs.ªª)ª¤
Keywords: algal limestone Qaidam Basin Qinghai Province
ª¤Tertiary of Chaixi area in Qaidam Basin developed algal-laminated, algal-stro matalite, algal-limestones are good hydrocarbon-bearing reservoirs, and the diss olution porosity of a little algal-micrites developed, which also formed hydroca rbon-bearing reservoirs. The former three algal-limestones are good hydrocarbon- bearing reservoirs, and the dissolution porosity of a little algal-micrites deve loped, which also formed hydrocarbon-bearing reservoirs. The distribution featur es of the algal-limestone are controlled by regional structure activities, lake horizontal face changes and paleogeology environments.
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ª¤20040272 Sun Mengru (Geology and Physical Geography Institute, Chinese Academy of Sc iences, Beijing); Zhang Qin Different Sedimentary Types of Clastic R ocks of the Paleogene in Dongying Sag, Shandong Province, China (Petroleum Explora tion an d Development, ª©ISSNªª1000-0747, ª©CNªª11-2360/P, 30(3), 2003, p.87-90, 4 ª©ill us.ªª, 4 tables, 9 ª©refs.ªª)ª¤
Keywords: clastic reservoirs Dongyi ng Depression Shandong Province
ª¤The Paleogene in Dongying sag developed different sedimentary types of petroc lastic reservoir rocks at the different stages of basin evolution, forming depos itional environments of alluvial fan, river, nearshore subaqueous fan, fan delta , deep water turbidite fan, delta, delta-front slump turbidite fan, and bar shor e-shallow lake. The reservoir rocks consisted of conglomerate, pebbly sandstone, medium-arenose sandstone, fine sandstone and siltstone. Different sedimentary t ypes of reservoir rocks have the different componential and textural maturities, of which delta-front mouth bar and bar shore-shallow lake reservoir sands have the highest componential and textural maturities.


ª¤ª¤20040273 Tan Mingyou (Geophysics Institute of Shengli Oilfield Company Limited, SINO EC, Dongying, Shandong); Analysis of the Early Tertiary Prototype B asin in the Dongying-Huimin Sag of the Bohaiwan Basin, China (Petroleum Geology & Experim ent, ª©ISSNªª1001-6112, ª©CNªª32-1151/TE, 25(4), 2003, p.348-352, 3 ª©illus.ªª, 8 ª©refs.ªª)ª¤
Keywords: sedimentary basins basin analysis Bohai Basin
ª¤Dongying-Huimin sag is located in the south of Jiyang Depression of the Bohai wan Basin. Commercial oil has been found in the Palaeocene and Lower Eocene Kong dian Formation. Hydrocarbon potential of Kongdian Formation is closely related t o the Early Tertiary basin prototype that controlled formation of oil and gas re servoirs. The prototype basin in that period was recognized as an extending half graben that was faulted in the north and onlapped in the south based on analysi s of tectonic evolution and sedimentary facies. The major controlling faults inc luded the north-northeast struck Ningnan fault, the western part of Wunan fault and Chennan fault. The Sichuan fault, the east part of Chennan fault and Wunan f ault that struck to northwest have also played a great part.
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ª¤20040274 Wang Jufeng (China University of Geosciences, Beijing); Cai X iyuan Evoluti on of Base-Level Cycles and Lithologic Traps of the Sha-3 Member in the Central Sag of the Dongying Depression, the Bohaiwan Basin, China (Petroleum G eology & Experiment, ª©ISSNªª1001-6112, ª©CNªª32-1151/TE, 25(4), 2003, p.357-361, 3 ª©i llus.ªª, 7 ª©refs.ªª)ª¤
Keywords: lithologic traps Dongying Depress ion Boahi Basin Shandong Province
ª¤The high-resolution sequence stratigraphical framework of Sha-3 member in the central sag of Dongying Depression has been established based on study of drill ing data and seismic data. The middle member of Sha-3 can be divided into one lo ng-term and six short-term of base level cycles. In accordance with the characte ristics of the base levels and the forming mechanism of the sandbody, the lithol ogic traps can be divided into three types: slump turbidite trap, slope-moving t urbidity fan trap and sublacustrine fan trap. The formation of traps was related to the evolution of base levels. The sub-lacustrine fan and slope-moving turbid ity fan which consisted of the main reservoirs were formed during rising stage o f the base level, and the slump turbidite was formed during the falling of base level.
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ª¤20040275 Wu Chaodong (School of Earth Space Science, Peking University , Beijing); Li u Jianmin The Reservoir Heterogeneity ad Analysis of Sedimentary Arc hitecture i n River Deposits (Chinese Journal of Geology, ª©ISSNªª0563-5020, ª©CNªª1 1-1937/P, 38(1) , 2003, p.60-73, 8 ª©illus.ªª, 2 tables, 24 ª©refs.ªª, with English abstract)ª¤
Keywords: reservoir Jitang Depression Shandong Province ª¤


ª¤20040276 Wu Huaguo (University of Petroleum, Shandong); Li Chun Ha line Lacustrine Biohermal Reservoir Characteristics in block Da 81-4 of the Yidong Oilfield, Ea st China (Petroleum Exploration and Development, ª©ISSNªª1000-0747, ª© CNªª11-2360/TE, 30(4), 2003, p.43-46, 4 ª©illus.ªª, 8 ª©refs.ªª)ª¤
Keywords: reefs reservoir Jiyang Depression Shandong Province
ª¤In Block Da 81-4 of the Yidong area, Jiyang Depression, bioherms in the Sha-4 Member of the Shahejie Formation were formed in haline lacustrine environment o n ramp margin. Five small scale bioherms are in vertical succession. Three major lithofacies associated with bioherms are: 1) dolomites dominate the lower algal reefs; 2) limestones comprise the majority of the algal knolls; and 3) limited presence of clastics and evaporates. Seven types of porosities are observed.

ª¤ª¤20040277 Wu Wenhui (State Key Laboratory of Oil and Gas Reservoir Geol ogy and Explor ation, Chengdu University of Technology, Chengdu, Sichuan); Huang Sijing Charac teristics of Petrology and Mineralogy of Reservoirs in Overpressure Basins (Jou rnal of Chengdu University of Technology (Science & Technology Edition), ª©ISSN ªª167 1-9717, ª©CNªª51-1634/N, 30(3), 2003, p.258-262, 3 ª©illus.ªª, 2 tables, 15 ª©re fs.ªª, with English abstract)ª¤
Keywords: clastic reservoirs sedime ntary petrology ª¥

ª¤20040278 Wu Yangyang (Department of Geology, Peking University, Beijin g); Feng Jun Advances in Research on Foreland Basin (Xinjiang Petroleum Geology, ª©I SSNªª1001-3 873, ª©CNªª65-1107/TE, 24(1), 2003, p.87-91, 4 ª©illus.ªª, 1 table, 17 ª©refs.ªª )ª¤
Keywords: foreland basins ª¥
ª¤A foreland basin is defined as a sedimentary basin deposited between frontal margin of orogenic belt and its adjacent craton. It can be divided into four str uctural elements such as wedge-top, foredeep, forebulge and back-bulge depo-zone s. There are three kinds of foreland basins classified in terms of origin and lo cation: peripheral foreland basin, retroarc foreland basin and regenerated forel and basin. The evolution of it is a dynamic process with the feature of progress ive development.
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ª¤20040279 Yuan Jing (University of Petroleum, Shandong); Du Yumin Probability Cumula tive Grain Size Curves in Terrigenous Depositional Environments of the Paleogene in Huimin Sag, Shandong Province, China (Petroleum Exploration and Dev elopmen t, ª©ISSNªª1000-0747, ª©CNªª11-2360/P, 30(3), 2003, p.103-106, 7 ª©illus.ªª, 15 ª©refs.ªª)ª¤
Keywords: clastic rocks sedimentary environment Huimi n Depression Shandong Province
ª¤A large number of probability cumulative grain size curves were plotted, and the probability cumulative grain size curves in the main sedimentary environment s of the Paleogene in Huimin sag were summarized on the basis of observation of cores. The distributary channels in delta plane subfacies are of typical bi-segm ent pattern and tri-segment pattern, those of the distributary channels in delta front subfacies of ¡°1 bouncing population-1 suspension population-transitional zone¡± pattern and ¡°low slope multi-segments¡± pattern. ª¤

ª¤20040280 Zhang Chuanlin (China University of Geosciences, Beijing); Zh ao Xingmin Sedimentary Characteristics and Reservoir Quality of Braided Deltas in Southern margin of Junggar Basin, Xinjiang, China (Xinjiang Petroleum Geology, ª©ISSNªª1001 -3873, ª©CNªª65-1107/TE, 24(3), 2003, p.202-204, 3 ª©illus.ªª, 1 table, 4 ª©refs .ªª)
Keywords: deltaic environment reservoir Junggar Basin Xinjiang
ª¤The braided deltas in southern margin of Junggar Basin as a significant type of sedimentary facies are mainly characterized by conglomerate, gravel sandstone and coarse-grained sandstone. The braided deltas, composed of the braid delta p lain, braid delta front and prodelta, are dominated by the braid delta plains. T he braid delta front sub-facies occupying the shallow lake is scoured by braid d istributary channel sandstone and undeveloped. On the other hand, the results fr om measuring the outcrop samples and the integrated petroleum geological analysi s show that the gravel sandstone body with better oil-gas accumulation is one of good reservoirs in this area. ª¤

ª¤20040281 Zhang Feng'e (Department of Water Resources and Environmental Engineering, China University of Geosciences, Beijing); Lu Yaoru Mechanism Relate d to the Fo rmation of Compound Karstification (Earth Science Frontiers, ª©ISSNªª100 5-2321, ª©CNªª1 1-3370/P, 10(2), 2003, p.495-500, 3 ª©illus.ªª, 3 tables, 18 ª©refs.ªª, with Eng lish abstract)ª¤
Keywords: karstification ª¥

ª¤ 20040282 Zhang Tonggang (Geological and Geophysical Institute, Chines e Academy of S ciences, Beijing); Chu Xuelei The Mixed Sedimentary Sequences of Ca rboniferous in Luobubo Area of Tarim Basin, Xinjiang, China (Xinjiang Petroleum Ge ology, ª©ISSNªª1001-3873, ª©CNªª65-1107/TE, 24(3), 2003, p.199-201, 1 ª©illus.ªª, 5 ª©r efs.ªª)
Keywords: Carboniferous Tarim Basin Xinjiang ª¥
ª¤The field outcrop section of Carboniferous in northern Luobubo sag of Tarim B asin was measured in detail. And the formation horizon was classified and correl ated basin on the paleontological feature, lithological and petrographic analyse s and stratigraphic analyses and stratigraphic correlation. It is confirmed from seismic trace and Luobei section connected to areal coverage that there exists Carboniferous sequence distributed within the areal coverage. The results show t hat in this typical sedimentary sequence, hydrocarbon source rocks and reservoir are fairly developed, which have great significance in petroleum geology; their probably favorable source-reservoir-cap assemblages mean better hydrocarbon pot entials in this area.
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ª¤20040283 Zhao Junxing (State Key Laboratory of Oil and Gas Reservoir G eology and Exp loitation, Chengdu University of Technology, Chengdu, Sichuan); Chen Hongde The Possibility of Rebuilding Paleogeomorphology before Basin Deposition by High-Re solution Sequence Stratigraphy (Journal of Chengdu University of Technol ogy (Sc ience & Technology Edition), ª©ISSNªª1671-9727, ª©CNªª51-1634/N, 30(1), 2003, p. 76-81, 4 ª©illus.ªª, 1 table, 7 ª©refs.ªª, with English abstract)ª¤ K eywords: sequence stratigraphy paleorelief ª¥

ª¤ 20040284 Zhao Zhongxin (China University of Geosciences, Wuhan, Hubei) ; Wang Hua Controlling Role of Fault-Break Zone on Sedimentary System¡ª¡ªTaking Qiongdongnan Ba sin as an Example (Petroleum Exploration and Development, ª©ISSNªª1000- 0747, ª©CNªª11-2360/P, 30(1), 2003, p.25-27, 4 ª©illus.ªª, 7 ª©refs.ªª)ª¤ Keywords: sedimentary system South China Sea
ª¥This paper identifi ed the major types of fault-break zones and their characte ristics based on concept of fault-break zones in Qiongdongnan Basin. And the aut hors respectively analyzed their control action on the depositional subarea and distributing of sedimentary sandbodies in Qiongdongnan Basin. Ultimately, the au thors summarized multilevel of fault-break zones and their controlling on spatia l distribution of sedimentary facies in different evolvement epoch in the Qiongd ongnan Basin. The fault-break zones not only controlled the changes of water-dep th and accommodation at the low-stand and high-stand periods, but also controlle d the distribution of sedimentary system and sedimentary system tracts of strata in the each depression of Qiongdongnan Basin.

ª¤ª¤20040285 Zheng Rongcai (State Key Laboratory of Oil and Gas Reservoir Geology and Ex ploitation, Chengdu University of Technology, Chengdu, Sichuan); Wang Chengshan Discovery of the First Example of ¡°White Smoke Type¡± of Exhalative Rock (Hydrot hermal Sedimentary Dolostone) in Jiuxi Basin and its Significance, Gansu Provinc e, China (Journal of Chengdu University of Technology (Science & Technol ogy Edi tion), ª©ISSNªª1671-9727, ª©CNªª51-1634/N, 30(1), 2003, p.1-8, 4 ª©illus.ªª, 13 ª©refs.ªª, with English abstract)
Keywords: dolodtone Jiuquan Bas in Gansu Province

ª¤20040286 Zhu Dagang (Institute of Geomechanics, Chinese Academy of Geo logical Scienc es, Beijing); Zhao Xitao Late Pleistocene Lacustrine-Beach Rock arou nd the Nam Co in Tibet, China (Geological Review, ª©ISSNªª0371-5736, ª©CNªª11-1952/ P, 49(4), 2003, p.432-438, 3 ª©illus.ªª, 1 plate, 2 tables, 28 ª©refs.ªª, with English abstract )
Keywords: lake sediments Upper Pleistocene Quaternay