玲珑金矿田构造蚀变岩带及找矿预测研究
|
摘要
位于山东省招远市的玲珑金矿田是我国重要的黄金生产基地,矿田内玲珑型花岗岩大面积出露,仅局部被第四系沉积物覆盖。控矿构造可分为两种类型,既压扭性和张扭性,前者控制着蚀变岩型矿体分布,后者则控制着含金石英脉型矿体分布。本文主要对矿田内两种类型构造蚀变岩带分布特征,矿化规律,形成年龄和岩石地球化学等方面进行研究,并在此基础上进行找矿预测。
研究表明:矿田内构造蚀变岩带主要有石英脉型和蚀变岩型两种,石英脉型构造蚀变岩带可划分为绢英岩带,钾化花岗岩带(包括强钾化花岗岩带和弱钾化花岗岩带)和未蚀变花岗岩带;蚀变岩型构造蚀变岩带亦可划分为绢英岩带,钾化花岗岩带(包括强钾化花岗岩带和弱钾化花岗岩带)和未蚀变花岗岩带。两者的差别在于所控制的矿体类型、蚀变规模和形成环境。控制石英脉型矿体的构造蚀变岩带规模较小,成矿时处于稳定和温度相对较低的氧化环境,化学组分以迁入为主,富集轻稀土元素;控制蚀变岩型矿体的构造蚀变岩带规模相对较大,形成时处于动荡和温度相对较高的还原环境,微量元素以迁入为主,富集重稀土元素。玲珑断裂带中钾长石蚀变年龄分布范围是69.47±0.9～110.3±1.0Ma,在成矿期间和成矿后都发生过强烈的运动,其中成矿期间的运动使后期热液再次叠加于早期品位较低的矿体上而形成工业矿体(如52号脉),成矿后的活动则是破坏早期形成的矿体,表现在西山和东山矿体的连续性在断裂带处被破坏。九曲矿区构造蚀变岩带蚀变年龄分布范围是90.35±0.88～99.49±1.01Ma,集中于90～100Ma,形成于玲珑金矿田大规模成矿的中晚期,三个蚀变岩分带均形成于同一期的成矿热液,且形成构造蚀变岩带时的成矿热液处于较低温阶段。
构造蚀变岩带岩相填图法可把矿山地质中几米～十几米的就矿找矿标志尺度发展到矿田级中尺度的大范围找矿标志和远矿的找矿标志,通过玲珑矿田的填图效果证明该方法在找矿预测中具有较强的实用性。通过预测和已有探矿工程证明玲珑矿田深部还存在可观的资源量,找矿远景最大的区域是NE向构造矿化富集带深部,矿化深度至少达到-1500米;其次是NNE向构造矿化富集带深部,矿化深度至少达到-1200米;再次是NEE向构造矿化富集带深部。
The Linglong ore-field which locates in Zhaoyuan City is the most important gold base in China, Shandong Province. The Linglong granite can be found in most areas and the Quaternary also can be found in some areas in the ore-field. The ore-control structure can be divided into two types which are transtension fracture and transpression fracture. The former controls quartz vein ore, and the latter controls altered rock ore. The purpose of this paper is to research the geological distribution, metallogenetic rules, age of alteration, and geochemical composition in two types of zoning of tectonic-alteration-facies, and then make prospecting forecast in Linglong gold field.
The study suggests that the tectonic-alteration-facies zoning can be divided into two types which are the quartz vein one and the altered rock one. The tectonic-alteration-facies zoning of quartz vein type includes the phyllic alteration zone, strongly potassic alteration granite zone, feebly potassic alteration granite zone and granite zone. The tectonic-alteration-facies zoning of altered rock type also includes the phyllic alteration zone, strongly potassic alteration granite zone, feebly potassic alteration granite zone and granite zone. The main differences between two types are the ore type, alteration scale and circumstances that formed. The alteration scale of tectonic-alteration-facies zoning which controlled the quartz vein ore is small, and it was formed in the circumstances that the ore-forming fluids was in middle-low temperature and oxidation, the chemical composition was moved into, and the LREE was enriched. The alteration scale of tectonic-alteration-facies zoneing which controlled altered rock ore is rare large, and it was formed in the circumstances that the ore-forming fluids was in middle-high temperature and deoxidization, the trace element composition was moved into, and the HREE was enriched. The alteration age of K-feldspar in Linglong fracture zone is 69.47±0.9～110.3±1.0Ma. The alteration age distribute shows that the faults moved during the metallization phase which the motion spurs ore-forming fluids superimposed mineralizing process and the postmineralization which the faults broke up the continuity of ore veins that formed in Xishan and Dongshan field. The alteration age of K-feldspar in Jiuqu is 90.35±0.88～99.49±1.01Ma, focus on 90～100Ma. The alteration age distribute shows that the three alteration zones were made from the co-hydrothermal fluids which stayed in middle-low temperature.
The traditional prospecting method always belongs to exploring ore by ore in a small rage. But the mapping method of tectonic-alteration-facies zoning provides us a suitable and big range prospect mark which can be used to explore buried ore. With the mapping method of tectonic-alteration-facies zoneing, we forecast much potential resource having been preservation in the deep area of Linglong field. The NE concentrated mineralization zone which the gold ore maybe found in the depth of 1500m is the first important place, the NNE concentrated mineralization zone which the gold ore maybe found in the depth of 1200m is the second important place, and the NEE is the third important place.
研究表明:矿田内构造蚀变岩带主要有石英脉型和蚀变岩型两种,石英脉型构造蚀变岩带可划分为绢英岩带,钾化花岗岩带(包括强钾化花岗岩带和弱钾化花岗岩带)和未蚀变花岗岩带;蚀变岩型构造蚀变岩带亦可划分为绢英岩带,钾化花岗岩带(包括强钾化花岗岩带和弱钾化花岗岩带)和未蚀变花岗岩带。两者的差别在于所控制的矿体类型、蚀变规模和形成环境。控制石英脉型矿体的构造蚀变岩带规模较小,成矿时处于稳定和温度相对较低的氧化环境,化学组分以迁入为主,富集轻稀土元素;控制蚀变岩型矿体的构造蚀变岩带规模相对较大,形成时处于动荡和温度相对较高的还原环境,微量元素以迁入为主,富集重稀土元素。玲珑断裂带中钾长石蚀变年龄分布范围是69.47±0.9～110.3±1.0Ma,在成矿期间和成矿后都发生过强烈的运动,其中成矿期间的运动使后期热液再次叠加于早期品位较低的矿体上而形成工业矿体(如52号脉),成矿后的活动则是破坏早期形成的矿体,表现在西山和东山矿体的连续性在断裂带处被破坏。九曲矿区构造蚀变岩带蚀变年龄分布范围是90.35±0.88～99.49±1.01Ma,集中于90～100Ma,形成于玲珑金矿田大规模成矿的中晚期,三个蚀变岩分带均形成于同一期的成矿热液,且形成构造蚀变岩带时的成矿热液处于较低温阶段。
构造蚀变岩带岩相填图法可把矿山地质中几米～十几米的就矿找矿标志尺度发展到矿田级中尺度的大范围找矿标志和远矿的找矿标志,通过玲珑矿田的填图效果证明该方法在找矿预测中具有较强的实用性。通过预测和已有探矿工程证明玲珑矿田深部还存在可观的资源量,找矿远景最大的区域是NE向构造矿化富集带深部,矿化深度至少达到-1500米;其次是NNE向构造矿化富集带深部,矿化深度至少达到-1200米;再次是NEE向构造矿化富集带深部。
The Linglong ore-field which locates in Zhaoyuan City is the most important gold base in China, Shandong Province. The Linglong granite can be found in most areas and the Quaternary also can be found in some areas in the ore-field. The ore-control structure can be divided into two types which are transtension fracture and transpression fracture. The former controls quartz vein ore, and the latter controls altered rock ore. The purpose of this paper is to research the geological distribution, metallogenetic rules, age of alteration, and geochemical composition in two types of zoning of tectonic-alteration-facies, and then make prospecting forecast in Linglong gold field.
The study suggests that the tectonic-alteration-facies zoning can be divided into two types which are the quartz vein one and the altered rock one. The tectonic-alteration-facies zoning of quartz vein type includes the phyllic alteration zone, strongly potassic alteration granite zone, feebly potassic alteration granite zone and granite zone. The tectonic-alteration-facies zoning of altered rock type also includes the phyllic alteration zone, strongly potassic alteration granite zone, feebly potassic alteration granite zone and granite zone. The main differences between two types are the ore type, alteration scale and circumstances that formed. The alteration scale of tectonic-alteration-facies zoning which controlled the quartz vein ore is small, and it was formed in the circumstances that the ore-forming fluids was in middle-low temperature and oxidation, the chemical composition was moved into, and the LREE was enriched. The alteration scale of tectonic-alteration-facies zoneing which controlled altered rock ore is rare large, and it was formed in the circumstances that the ore-forming fluids was in middle-high temperature and deoxidization, the trace element composition was moved into, and the HREE was enriched. The alteration age of K-feldspar in Linglong fracture zone is 69.47±0.9～110.3±1.0Ma. The alteration age distribute shows that the faults moved during the metallization phase which the motion spurs ore-forming fluids superimposed mineralizing process and the postmineralization which the faults broke up the continuity of ore veins that formed in Xishan and Dongshan field. The alteration age of K-feldspar in Jiuqu is 90.35±0.88～99.49±1.01Ma, focus on 90～100Ma. The alteration age distribute shows that the three alteration zones were made from the co-hydrothermal fluids which stayed in middle-low temperature.
The traditional prospecting method always belongs to exploring ore by ore in a small rage. But the mapping method of tectonic-alteration-facies zoning provides us a suitable and big range prospect mark which can be used to explore buried ore. With the mapping method of tectonic-alteration-facies zoneing, we forecast much potential resource having been preservation in the deep area of Linglong field. The NE concentrated mineralization zone which the gold ore maybe found in the depth of 1500m is the first important place, the NNE concentrated mineralization zone which the gold ore maybe found in the depth of 1200m is the second important place, and the NEE is the third important place.
引文
[1] Bierlein F P et al.Origin of hydrothermal Cu-Zn-Pb minerlisation in the Olary Block,south Astralia:evidence from fluid inclusions and sulphur istopes[J]. Precambrian Research, 1996,79(3～4):281～305.
[2] Campbell Mccuaig T. P-T-deformation-fluid characteristics of lode gold deposits: evidence from alteration system [J]. Ore Geology Review,1998,12(6):381～454.
[3] Deng Jun,Fang Yun,Wan Li et al.Fuzzy comprehensive appraisal of concealed ore deposit [J].Journal of China University of Geosciences,2000,11(2):134～139.
[4] Deng Jun,Fang Yun,Yang Liqiang,et al.Numerical modeling of ore-forming dynamics of fractal dispersive fluid systems [J].Acta Geologica Sinica,2001,75(2):220～232.
[5] Deng Jun, Yang Liqiang, Zhai Yusheng.Crust-mantle interaction and dynamics of metallogenic system of Jiaodong gold ore concentrating area, China [J]. Journal of Geosciences of China, 1999, 1(1): 39～46.
[6] Deng Jun, Zhai Yusheng, Wang Jingping,et al. Shear Alteration, Mass Transfer and Gold Mineralization: An Example from Jiaodong Ore Deposit Concertrating Area, Shangdong, China [J]. Journal of China University of Geosciences, 2000, 11(3):281～287.
[7] Deng Jun, Wang Qingfei, Sun Zhongshi. Origin of gold-bearing fluid and its initiative localization mechanism in Xiadian gold deposit, Shandong province [J]. Chinese Journal of Geochemistry,2002, 21(3): 282～288.
[8] Deng Jun, Liu Wei, Sun Zhongshi, et al. Evidence of mantle rooted fluids and multi-level circulation ore-forming dynamics: A case study from the Xiadian gold deposit, Shandong province, China [J]. Science in China (Series D), 2003, 46 (Sup): 123～134.
[9] Deng Jun, Yang Liqiang, Sun Zhongshi, et al. A metallogenic model of gold deposits of the Jiaodong granite-greenstone belt [J]. Acta Geologica Sinica, 2003, 77 (4): 537～546.
[10] Deng Jun, Wang Qingfei, Wei Yanguang, et al. Metallogenic effect of transition of tectonic dynamic system [J].Journal of China University of Geosciences, 2004, 15(1): 23～28.
[11] Deng Jun, Huang Dinghua, Wang Qingfei,et al.Surplus space method: A new numerical model for prediction of shallow-seated magmatic bodies [J].Acta Geologica Sinica, 2004,78(6):1245～1249.
[12] Deng Jun, Yang Liqiang, Ge Liangsheng, et al. Research advances in the Mesozoic tectonic regimes during the formation of Jiaodong ore cluster are [J]. Progress in matural science, 2006, 16(8): 777～784.
[13] Deng J,Yang L Q,Sun Z S,et al.A metallogenic model of gold deposits of the Jiaodong granite-greenstone belt[J].Acta Geologica Sinica.2003a,77(4):537～546.
[14] Eilu P,Mikucki E J,Dugdale A L.Alteration zoning and primary geochemical dispersion at the Bronzewing lode-gold deposit,Western Australia[J].Mineralium Deposita,2001, 36:13～31.
[15] Fan H R, Zhai M G, Xie Y H,et al.Ore-forming fluids associated with granite hostedgold mineralization at the Sanshandao deposit,Jiaodong gold province,China[J]. Mineralium Deposita,2003,38:739～750.
[16] ferences from San Gabriel fault rock geochemistry and microstructures[J].J G R,100(B7),1995,13007～13020.
[17] Grant J A. The isocon diagram-a simple solution to Gresens' equation for metasomatic alteration[J].Economic Geology,1986,81:1976～1982.
[18] Gresens R L.Composition-volume relation of metasonatism[J].Chemical Geology,1967, 2:47～55.
[19] James P Evans,Frederick Mchester.Fluid-rock interaction in the San Andres system:in ferences from San Gabriel fault rock geochemistry and microstructures[J].J G R,100(B7),1995,13007～13020.
[20] John Ridley.The relations between mean rock stress and fluid flow in the crust: with reference to vein-and lode-style gold deposit[J]. Ore Deposit Review,1993:23～37.
[21] Jones M E J.Struct.Geol.,1981,3(3):333～338.
[22] Kieran D.Fluid-rock interaction in crustal shear zone:a directed percolation approach[J].Geology,1994,22:843～846.
[23] Leitch C H B,Lentz D R.The Gresens approach to mass balance constraints of alteration systems:Methods,pitfalls,examples[A].In:Lentz D R.Alteration and Alteration Process- es As-sociated with Ore-Forming Systems(Vol.11)[C].Waterloo:Geological Association of Canada,1994.161～192.
[24] MacLean W H,Kranidiotis P.Immobile elements as monitorsof mass transfer in hydroth- ermal alteration: Phelps Dodgemassive sulphide deposit,Matagami,Quebec[J].Econ- omic Geology,1987,82:951～962.
[25] MacLean W H.Mass change calculations in altered rock series[J].Mineralium Deposita, 1990,25:44～49.
[26] Maclntyer D G.Sedex-sedimentary-exhalative deposit, ore deposits,tectonics and metalogeny in the Canadian Cordillera.Ministry of Energy,Mines and Petroleum Resources, British Columbia, Queen’s Printer for British Columbia[M].Victoria: 1995: 5～20.
[27] Madeisky H E, Stanley C R.Lithogeochemical exploration ofmetasomatic zones associ- ated with volcanic-hosted massivesulfide deposits using Pearce Element Ratio analysis[J]. Inter national Geology Review,1993,35:1121～1148.
[28] Mandelbort B.B. Fractals: Form, Chance and Dimension.FreemanSan, Francisco, 1977.
[29] Mandelbort B.B. The Fractal Geometry of Nature.Freeman, San Francisco, 1982.
[30] Parry W T. Fault-fluid compositions from fluid-inclusion observations and solubilities of fracture-sealing minerals[J]. Prcambrian Research,1998,290(1～2):1～26.
[31] Sibson R H .Crustal stress, faulting and fluid flow[A].Parnell J, ed. Geological Special publications[C].Bath,The Geological Special publications House, 1994,69～84.
[32] Sibson R H.Fault rocks and fault mechanisms[J].J Geol.Soc.London,1977,133:191～213.
[33] Yang J H,Zhou X H. The Rb-Sr isochron of ore and pyrite subsamples from Linglong gold deposit,Jiaodong Peninsula,eastern China and their geological signi-ficance[J]. Chinese Sci.Bull,2000,45:2272～2276.
[34] Yang J H,Zhou X H.Rb-Sr,Sm-Nd and Pb isotope systematics of pyrite:implications for the age and genesis of lode gold deposits[J]. Geoloy,2001,29:711～714.
[35] Yang L Q,Deng J,Zhang J,et al.Preliminarystudies of Fluid Inclusions in Damoqujia Gold Deposit along Zhaoping Fault Zone,Shandong province,China[J].Acta Petrologica Sinica,2006,23(1):1～10.
[36] Zwart, H J. On the determination of polymorphic mineral associations and its application to the Bosost area (central phrenees)[J].Geol.Rundschau,1962,52:38～65.
[37] Zwart, H J. Some examples of the relations between deformation and metamorphism from the central Phrenees[J].Geol.en Mijinbouw.1963,42:143～154.
[38]岑况,钟玉芳.攀西地区基性超基性岩地球化学及嵌套韵律层的分形动力学研究[J].现代地质, 1999,13(4):408～410.
[39]陈春仔,金友渔.分形理论在成矿预测中的应用[J].矿产与地质,1997,11(4):272～275.
[40]陈光远,孙岱生,邵伟.胶东金矿成因矿物学与找矿[M].重庆出版社,1989,1～452.
[41]陈国达.成矿构造研究法.北京:地质出版社,1978.
[42]陈衍景,Pirajno F,赖勇,等.胶东矿集区大规模成矿时间和构造环境[J].岩石学报,2004,20(4):907～922.
[43]陈毓川,裴荣富,宋天锐,等.中国矿床成矿系列:第五届全国矿床会议论文集[C].北京:地质出版社,1993:89～90.
[44]陈毓川.矿床的成矿系列[J].地学前缘,1994,1(3-4):90～9.
[45]陈远荣,贾国相,徐庆鸿.元素集成快速定位预测隐伏矿的新技术研究[M].地质出版社,2003.
[46]陈远荣.有机烃气新方法寻找有色、贵金属矿床的研究:[博士学位论文].湖南长沙:中南大学,2001.
[47]成秋明.成矿过程奇异性与矿产预测定量化的新理论与新方法[J].地学前缘,2007,14(5):42～53.
[48]成秋明.非线性成矿预测理论:多重分形奇异性-广义自相似性-分形谱系模型与方法[J].地球科学-中国地质大学学报,2006,31(3):337～348.
[49]程裕琦,陈毓川,赵一鸣,等.再论矿床地成矿系列问题-兼论中生代某些矿床地成矿系列[J].地质论评,1983,29(2):127～139.
[50]寸珪,陈纪明.中华人民共和国黄金矿产图集[M].廊坊:国家黄金管理局黄金地质研究所,1992,65.
[51]邓军,张国铎,孙希贤.胶东半岛招掖金矿带控矿构造特征及灰色领域初探[J].中国区域地质,1993,(3):264～273.
[52]邓军,孙希贤.隐形类矿床的灰色特征及其灰色预测初探[C].见:何科昭主编.献给校庆四十周年文集.北京:海洋出版社,1993,217～223.
[53]邓军.山东招掖金矿带断裂构造分带与蚀变矿化分带关系研究[J].矿床地质,1994,13:17～19.
[54]邓军,徐守礼,孙希贤.模糊数学在胶东西部金矿带成矿预测研究中的应用[J].现代地质,1994, 8(2):229～235.
[55]邓军,方云,周显强.山东胶西北金矿带成矿构造应力场反演及其控矿作用[J].中国区域地质,1995,(3):252～260.
[56]邓军,方云,周显强,等.胶东半岛西北部金矿带成矿构造应力场及成矿微量元素分布特征研究[J].地球学报,1995,(1):10～21.
[57]邓军,徐守礼,吕古贤,等.胶东西北部断裂构造与成矿作用研究[J].现代地质,1996,10(4): 502～511.
[58]邓军,吕古贤,杨立强,等.构造应力场转换与界面成矿[J].地球学报,1998,19(3): 244～250.
[59]邓军,翟裕生,杨立强,等.论剪切带构造成矿系统[J].现代地质,1998,12(4): 493～500.
[60]邓军,杨立强,孙忠实,等.剪切带构造成矿动力机制与模式[J].现代地质,1999,13(2):125～129
[61]邓军,翟裕生,杨立强,等.剪切带构造-流体-成矿系统动力学模拟[J].地学前缘,1999,6(1),115～126.
[62]邓军,翟裕生,杨立强,等.构造演化与成矿系统动力学-以胶东金矿集中区为例[J].地学前缘,1999,6(2): 315～323.
[63]邓军,杨立强,方云,等.胶东地区壳-幔作用与金成矿效应[J].地质科学,2000,35(1): 60～70.
[64]邓军,杨立强,孙忠实等.构造体制转换与流体多层循环成矿动力学[J].地球科学,2000,25(4): 397～403.
[65]邓军,杨立强,方云等.成矿系统嵌套分形结构与自有序效应[J].地学前缘,2000,7(1): 133～146.
[66]邓军,杨立强,孙忠实等.矿源系统地质-地球化学例析[J].现代地质,2000,14(2): 165～172.
[67]邓军,杨立强,翟裕生,等.构造-流体-成矿系统及其动力学的理论格架与方法体系[J].地球科学,2000,25(1):71～78.
[68]邓军,方云,杨立强,等.剪切蚀变带与物质迁移及金的富集-以胶东矿集区为例[J].地球科学,2000,25(4): 428～432.
[69]邓军,孙忠实,杨立强,等.成矿流体运动系统与金质来源和富集机制讨论[J].地质科技情报,2000,19(1):41～45.
[70]邓军,王建平,王建国,等.胶东半岛西北部金矿带构造动力控矿[C].中国金都招远国际金矿地质与勘查学术论坛论文集,地震出版社,2002:55～58.
[71]邓军,王庆飞,孙忠实,等.矿物磁性与金元素富集的可能关系[J],现代地质,2002,16(2):177～179.
[72]邓军,孙忠实,候增谦,等.板块界面磁斥力形成与全球大型-超大型金矿分布规律初探[J].地质科学,2002,37(4):502～508.
[73]邓军,王庆飞,杨立强,等.胶西北金矿集区成矿作用发生的地质背景[J].地学前缘,2004, 11(4):527～533.
[74]邓军,王庆飞,黄定华.成矿流体运输物理机制研究的关键难题与方法体系[J].地球科学进展, 2004,19(3):393～398.
[75]邓军,王庆飞,杨立强,等.胶东西北部金热液成矿系统内部结构解析[J].地球科学,2005,30(1): 102～108.
[76]邓军,杨立强,葛良胜,等.胶东矿集区形成的构造体制研究进展[J].自然科学进展,2006,16(5): 513～518.
[77]邓军,杨立强,王庆飞,等.胶东矿集区金成矿系统组成与演化概论[J].矿床地质,2006,25: 67～70.
[78]丁汝福,王京彬,蔡新平,等.成矿作用研究结合综合方法技术预测隐伏金矿[J].矿产与地质,17(6):669～672.
[79]丁式江,翟裕生,邓军.胶东焦家金矿蚀变岩中元素的质量迁移[J].地质与勘探,2000,36(4):28～31.
[80]都城秋惠.变质作用与变质带[M],周云生译(1979),地质出版社,1972,1～492.
[81]范永香.初论内生金属矿床矿区地质预测的主要途径[J].地球科学,1984,4:107～116.
[82]高帮飞,邓军,王庆飞,等.风化作用元素迁移与金富集机制研究-以国内外典型红土型金矿床为例[J].黄金,2006,27(5):9～12.
[83]耿文辉,敬荣中,韦龙明,等.有色金属矿山可持续发展找矿预测方法与应用[J].矿产与地质,2004,18(104):350～355.
[84]贡恰罗夫,M.A.等.变形-化学共生组合与构造-变质分带[J].国外地质科技,1996,(31):48～53.
[85]关康,罗镇宽,苗来成,等.郭家岭型花岗岩地球化学特征与金矿化的关系[J].地质找矿论丛,1997,12(4):1～8.
[86]哈本海,武际春,戴立新,等.玲珑金矿田控矿断裂-矿化特征及成矿远景展望[J].黄金(增刊),2006,27:54～57.
[87]韩润生.初论构造成矿动力学及其隐伏矿定位预测研究内容和方法[J].地质与勘探,2003,39(1):5～9.
[88]郝广成,常和平.成矿有利度分析方法在山东平邑铜石南部地区金矿综合信息成矿预测中的应用[J].山东地质,2002,18(2):16～19.
[89]洪岩,邓永高,孔庆存,等.山东招远玲珑金矿田构造控矿规律及深部成矿预测(科研报告).1987,1～48.
[90]胡世玲.山东玲珑和郭家岭岩体的同位素年龄及其地质意义[J].岩石学报,1987,(3):83～89.
[91]胡受奚,赵懿英,徐金方,等.华北地台金矿地质[M].北京:科学出版社,1997,220.
[92]姜维明,哈本海,王启梁,等.玲珑金矿田九曲-大开头矿段深部矿体定位分析[J].黄金科学技术,2004,12(4):17～21.
[93]敬荣中,鲍光淑,郭仁敏.矿山可持续发展综合物探技术方法研究[J].矿产与地质,2002,16(3):187-190.
[94]敬荣中,鲍光淑,林剑,等.一种基于数据融合的地球物理数据联合反演方法-以VES和MT为例[J].地球物理学报,2004,47(1): 143-150.
[95]敬荣中,鲍光淑,周屹.坑道综合物探方法在生产矿山中的应用[J].中南工业大学学报,2000(1):4-8.
[96]科兹洛夫斯基,E.A.科拉超深钻井(上)[M],张秋生主译(1991).地质出版社,1984,1～218.
[97]孔庆存,宋玉国,邓永高,等.玲珑金矿田矿脉深部成矿预测方法[J].地质找矿论丛,1987,2(4):77～83.
[98]孔庆存,宋玉国,邓永高,等.山东招远玲珑金矿构造控矿规律及深部成矿预测[C].国际金矿地质与勘探学术会议论文集:东北工学院出版社,1989,385～388.
[99]李东旭,周济元.地质力学导论[M].地质出版社,1986,1～343.
[100]李洪玉,姜振富.玲珑金矿田双顶矿段地质特征及金的富集规律[J].黄金,1999,20(11):9～11.
[101]李厚民,毛景文,沈远超,等.胶西北东季金矿床钾长石和石英的Ar-Ar年龄及其意义[J].矿床地质,2003,22(1):72～77.
[102]李华芹.刘家齐,魏琳.热液矿床流体包裹体年代学研究及其地质应用[M].北京:地质出版社,1993. 125～126
[103]李俊建,罗镇宽,刘晓阳,等.玲珑金矿区成矿后花岗斑岩脉的锆石SHRIMP U-Pb年龄对胶北地体演化的制约[J].2005,12(2):317～323.
[104]李士先,刘连生.山东胶西北S型构造及其对金矿的控制作用[J].地质力学文集,1981,5:38～57.
[105]李树勋,刘喜山.韧性剪切变质带特征及与金矿化的关系[J].1988,(5):19～21.
[106]李四光.关于地质构造的三个基本概念[J].地质学报,1953,33(4):233～260.
[107]李荫清,芮宗瑶,程莱仙.玉龙斑岩铜(钼)矿床的流体包裹体及成矿作用研究[J].地质学报,1981,55(3):216～231.
[108]李兆龙,杨敏之.胶东金矿床地质地球化学[M].天津科学技术出版社,1993,1～292.
[109]林文蔚,殷秀兰.成矿流体的浓缩作用及浓缩方式研究[J].地球学报,1998,19(2): 158～165.
[110]林文蔚,殷秀兰.胶东金矿成矿流体同位素的地质特征[J].岩石矿物学杂志,1998,17(3):249～259.
[111]刘瑞珣.显微构造地质学[M].北京大学出版社,1988,1～235.
[112]刘石年.山东玲珑式金矿床矿体空间定位形式及其形成机制的探讨[J].地球科学,1884,(4):47～56
[113]刘志刚.玲珑金矿田控矿构造研究[J].长春地质学院学报,1983,(3):47～54.
[114]卢焕章,Guy Arcambault,李院生,等.山东玲珑一焦家地区形变类型与金矿的关系[J].地质学报,1999,73(2):174～190.
[115]卢焕章,J Guha,方根保.山东玲珑金矿的成矿流体特征[J].地球化学,1999,28(5):421～437.
[116]卢焕章,袁万春,张国平,等.玲珑—焦家地区主要金矿床稳定同位素及同位素年代学[J].桂林工学院学报,1999,19(1):1～8.
[117]吕古贤,邓军,郭涛,等.玲珑-焦家式金矿构造变形岩相形迹大比例尺填图与构造成矿研究[J].地球学报,1998,19(2):177～186.
[118]吕古贤,郭涛,刘杜鹃.玲珑-焦家式金矿构造地质特征及成矿构造物理化学参量因子分析-以阜山金矿区为例[J].地球学报,2002,23(5):409～416.
[119]吕古贤,郭涛,舒斌,等.构造变形岩相形迹的大比例尺填图及其对隐伏矿床地质预测-以胶东玲珑-焦家式金矿为例[J].中国区域地质,2001,20(3):313～321.
[120]吕古贤,郭涛.阜山金矿区构造变形岩相特征与成矿流体构造物理化学特征研究[J].矿床地质(增刊),1998,(17):939～942.
[121]吕古贤,侯成桥,郭涛,等.玲珑金矿田深部资源第二富集带的预测研究[J].黄金(增刊),2006,27:47～53.
[122]吕古贤,孔庆存,邓军,等.山东玲珑和焦家金矿成矿深度研究与测算[J].地质论评,1996,42(6): 550～559.
[123]吕古贤,孔庆存.胶东玲珑-焦家式金矿地质[M].北京:科学出版社,1993,1～253.
[124]吕古贤,李晓波,倪师军,等.构造物理化学研究的一个重要问题-“构造附加静水压力”及其应用[J].华南地质与矿产,1998,56(4):1～13.
[125]吕古贤,林文蔚,郭涛,等.金矿成矿过程中构造应力场转变与热液浓缩-稀释作用[J].地学前缘,2001,8(4):253～264.
[126]吕古贤,林文蔚,罗元华,等.构造物理化学与金矿成矿预测[M],北京:地质出版社,1999,1～458.
[127]吕古贤,刘瑞珣,王方正,等.成岩成矿深度构造校正测算和实测[J].地质力学学报,2000,6(3): 50～62.
[128]吕古贤,刘瑞珣,王方正,等.成岩成矿深度构造校正测算和实例[J].地质力学学报,2000,6(3):50～62.
[129]吕古贤,刘瑞珣.重力和构造力在地壳中的作用.高校地质学报,1996,2(1):28～37.
[130]吕古贤、邓军、郭涛,等.玲珑-焦家式金矿构造变形岩相形迹大比例尺填图与构造成矿研究[J].地球学报,1998,19(2):177～186.
[131]吕古贤.构造物理化学的研究与应用[J].中国地质,1997,10:45～48.
[132]吕古贤.构造物理化学基本问题与金矿成矿预测[J].地球学报,1998,19(2):117～125.
[133]吕古贤.关于构造物理化学的初步探讨[J].中国区域地质,1991,(3):254-261.
[134]吕古贤.关于构造作用力影响“静水压力”问题[J].科学通报,1995,40(3):286.
[135]吕古贤.胶东半岛构造-岩相形式及玲珑-焦家式金矿的构造动力成岩成矿地质特征研究[J].中国地质科学院院报,1991,23:23～42.
[136]吕古贤.胶东半岛构造-岩相型式及玲珑-焦家式金矿的构造动力成岩成矿地质特征研究[J].中国地质科学院院报,1991b,(23):65～80.
[137]吕古贤.胶东玲珑-焦家式金矿床矿源岩系系列研究[J].矿床地质,1998,17:935～938.
[138]吕古贤.山东玲珑金矿田和焦家金矿田成矿深度的测算与研究方法[J].中国科学(D辑),1997, 27(4):337～342.
[139]吕古贤.山东省玲珑金矿田成矿深度的研究与测算[J].科学通报,1995,40(15): 1399～1402.
[140]罗镇宽,苗来成.胶东招莱地区花岗岩和金矿床[M].冶金工业出版社,2002,1～143.
[141]骆万成,伍勤生.应用蚀变矿物测定胶东金矿的成矿年龄[J].科学通报,1987,33:(6):1245～1248.
[142]马丽芳(主编).中国地质图集[M].北京:地质出版社,2002,348.
[143]马托埃,W.地壳变形[M],孙坦,张道安译(1984).地质出版社,1980,1～339.
[144]苗来成,罗镇宽,黄佳展,等.山东招掖金矿带内花岗岩类侵入锆石SHRIMP研究及其意义.中国科学, D辑,1997,27(3): 207～213.
[145]帕塔拉哈,E. U.构造相分析,产生与发展[J].国外地质科技,1987,(5).
[146]钱建平.构造动力成矿理论若干问题的探讨[J].地质地球化学,2002,30(4):1～6.
[147]裘有守,王孔海,催克英,等.山东牟平-乳山地区变质岩和花岗岩含金性及其与金矿成矿关系-中国金矿主要类型区域成矿条件文集(胶东地区)[M].地质出版社,1988,120～174.
[148]裘有守,王孔海,杨广华,等.山东招远-掖县地区金矿区域成矿条件[M].辽宁科学技术出版社,1988,1～291.
[149]申维.分形混沌与矿产预测[M].北京:地质出版社,2002.
[150]申玉科.胶西北金矿集中区构造-蚀变网络研究:[博士学位论文].北京:中国地质大学(北京),2006:1～101.
[151]孙国胜,李绪俊,姚凤良,等.玲珑金矿田矿物组合与地球化学分带及矿体定位预测意义[J].地质与勘探,2002,38(4):28～32.
[152]孙国胜,姚凤良,胡瑞忠,等.玲珑金矿田矿体富集规律及其控制因素[J].大地构造与成矿学,2001,25(4):464～470.
[153]孙景运.胶东玲珑金矿田52号脉群成矿规律及其找矿应用[J].地质地球化学,1985,(1):71～73.
[154]孙景运,周炳煌,王金城,等.山东玲珑金矿田东山矿床构造控矿规律及其在找矿勘探上的应用[C].国际金矿地质与勘探学术会议论文集,东北工学院出版社,134～135.
[155]孙启祯.边缘成矿与成矿预测[C]∥陈毓川,主编.当代地质矿产资源勘查评价的理论与方法.北京:地震出版社,1999:26～33.
[156]万丽,王庆飞,高帮飞,等.成矿预测数据统计方法[J].现代地质,2005,19(4):615～620.
[157]万丽,王庆飞,高帮飞.成矿预测中的非线性数学方法[J].地质找矿论丛,2006,21(1):45～48.
[158]汪劲草,王国富,汤静如.玲珑-焦家地区金矿成矿构造体制的新认识[J].桂林工学院学报,2002,22(1):1～4.
[159]王鹤年,汪耀,陈延安.胶东中元古代玲珑花岗岩及其后期叠加改造作用的地质、地球化学证据[J].南京大学学报(地球科学版),(1):105～118.
[160]王继伦,李善芳,齐文秀.中国金矿物探、化探方法技术的研究与应用[M].北京:地质出版社,1997.
[161]王林祥.沂沐断裂带内构造体系特征及其复合现象[J].长春地质学院学报,1987,17(1):11～20.
[162]王明志,李闫华,鄢云飞,等.若干成矿预测理论研究综述[J].资源环境与工程,2007,21(4):363～369.
[163]王仁铎,杨明国.地质现象分形统计学研究的若干问题[J].现代地质,1998,12 (1):91～98.
[164]王秀璋,程景平.我国某些层控矿床的成矿时差和时控特征-地球化学文集[M].科学出版社,1986,14～20.
[165]王中刚,于学元,赵振华,等.稀土元素地球化学[M],科学出版社,1989,76～94
[166]韦龙明,吴烈善,李惠,等.若干类型金矿找矿方法评述与综合找矿模型[J].桂林工学院学报,2003,23(1):5～9.
[167]吴烈善,韦龙明.有机烃新方法在金矿床快速定位预测中的应用:以陕西八卦庙特大型金矿床为例[J].地球化学,2001,30(6):579～584.
[168]谢尔曼,С.И.地壳断裂发育的物理规律[M],高中和译(1980).地震出版社,1977,,1～209.
[169]徐金方.玲珑复式花岗岩基的构成及其形成时代[J].岩石学报,1991,(2):43～49.
[170]杨进辉,周新华.胶东地区玲珑金矿矿石和载金矿物Rb-Sr等时线年龄与成矿时代[J].科学通报,2000,45(14):1547～1552.
[171]杨开庆.关于构造控岩控矿与构造成岩成矿问题[J].地质力学论丛,北京:科学出版社,1982,(6):9～19.
[172]杨敏之,李治平.胶东东部金青顶金矿床围岩蚀变的地球化学、形成机理及找矿方向[J].地质找矿论丛,1989,4(2):1～17.
[173]杨敏之,吕古贤.胶东绿岩带金矿地质地球化学[M].北京:地质出版社,1996.1～221.
[174]杨敏之.金矿床围岩蚀变带地球化学-以胶东为例[M].北京:地质出版社,1998,1～120.
[175]杨士望.论胶东半岛西北部胶东群地层、金的矿源层和金矿床的层控性质[J].地质找矿论丛,1986,1(2):1～12.
[176]杨士望.论胶东半岛西北部胶东群地层、金的矿源层和金矿床的层控性质[J].地质找矿论丛,1986,1(3):39～48.
[177]杨世瑜,钟昆明.北衙斑岩型金矿床快速定位预测-影像线环结构-构造地球化学集成成矿预测方法[J].中国工程科学(增刊),2005,7:224～227.
[178]杨新岳,谢国源,李志纯.变形过程中的流体—岩石作用和变形岩石质量平衡[J].中国科学(B辑),1995,25(3):329～336.
[179]杨岳衡,刘铁兵,李厚民.多元素X射线荧光分析方法在山东郭城金矿成矿预测中的应用[J].黄金科学技术,2000,8(5):13～19.
[180]杨忠芳,徐景奎,赵伦山,等.胶东两大成因系列金矿石英包裹体氮氧同位素及成矿流体组分地球化学研究[J].矿物学报,1991,11(4):363～369.
[181]姚凤良,刘连登,孔庆存,等.胶东西北部脉状金矿[M].吉林科学技术出版社,1990,1～234.
[182]翟裕生,邓军,李晓波,等.区域成矿学[M].北京:地质出版社,1999:154～171.
[183]翟裕生,彭润民,邓军,等.成矿系统分析与新类型矿床预测[J].地学前缘,2000,7(1):123～132.
[184]翟裕生,熊永良.关于成矿系列的结构[J].地球科学,1987,12(4):375～380.
[185]翟裕生,姚书振,等.成矿系列研究[M].武汉:中国地质大学出版社,1996:1～28.
[186]翟裕生.成矿系列研究问题[J].现代地质:中国地质大学研究生院学报,1992,6(3):300～307.
[187]翟裕生.关于构造-流体-成矿作用研究的几个问题[J].地学前缘1996,3(4):230～236.
[188]翟裕生.论成矿系统[J].成矿前缘,1999,6(1):13～27.
[189]战传富.郊庐断裂带强震活动的深部构造标志[J].地震地质,1983,5(1):42～52.
[190]张德宏,张庆禧.玲珑金矿田岩石地球化学测量及其找矿效果[J].山东地质,1998,14(1):47～52.
[191]张均,周乔伟.分形方法在金矿化时空结构分析中的应用[J].现代地质,2000,14(1):56～60.
[192]张可清,杨勇.蚀变岩质量平衡计算方法介绍[J].地质科技情报,2002,21(3):104～107.
[193]张理刚.稳定同位素在地质科学中的应用[M].陕西科学技术出版社,1985,1～267.
[194]张儒瑗,从柏林.矿物温度计和矿物压力计[M].地质出版社,1983.
[195]张生,李统锦,陈义兵.长坑矿床矿化过程中元素的质量迁移及金银关系[J].地质找矿论丛,1997,12(3):33～40.
[196]张渊,王微,王威.玲珑金矿田矿石学研究[J].世界地质,1995,14(3):39～42
[197]张远飞,吴健生.基于遥感图像提取矿化蚀变信息[J].有色金属矿产与勘查,1999,8(6): 604～606.
[198]张振海,张景鑫,叶素芝.胶东金矿同位素年龄厘定[M].北京地质出版社,1994.
[199]张振海.胶东招-掖金矿带等时线的研究及测定[J].贵金属地质,1993,2(1):26～33.
[200]赵鹏大.“三联式”资源定量预测与评价[J].地球科学,2002,27(5):482～489.
[201]赵希溦.矿物中包裹体的显微镜下研究及其在地质研究中的作用[J].长春地质学院学报,1981,(4):38～46.
[202]赵震宇,王世称,许亚明,等.综合信息矿产预测理论在危机矿山资源预测中的应用思考[J].世界地质,2000,21(3):283～286.
[203]钟增球,游振东.剪切带的成分变异及体积亏损-以河台剪切带为例[J].科学通报,1995,40(10):913～916.
[204]周凤英,李兆麟.胶东台上金矿床矿物中包裹体研究[J].矿物学报,1991,11(4):403～413.
[205]周国发,吕古贤,申玉科,等.山东大庄子金矿Ⅰ号脉构造蚀变带特征及其地质意义[J].黄金,2008,29(12):7～10.
[206]周奇明,赵友方,黄华鸾,等.电吸附法寻找隐伏矿床的试验研究[J].地质与勘探,2001,(2)69～73.
[207]朱奉三.混合岩化热液型金矿床成矿作用初步研究-以招掖地区的金矿床为例[J].地质与勘探,1980,7:1～9.
[208]朱裕生,梅燕雄.成矿模式研究的几个问题[J].地球学报,1995,2:182～18.
[209]朱作山,任英忱.应用数理统计方法研究玲珑、焦家两种类型金矿床的成因[J].地质找矿论丛,1988,3(3):72～78.
[2] Campbell Mccuaig T. P-T-deformation-fluid characteristics of lode gold deposits: evidence from alteration system [J]. Ore Geology Review,1998,12(6):381～454.
[3] Deng Jun,Fang Yun,Wan Li et al.Fuzzy comprehensive appraisal of concealed ore deposit [J].Journal of China University of Geosciences,2000,11(2):134～139.
[4] Deng Jun,Fang Yun,Yang Liqiang,et al.Numerical modeling of ore-forming dynamics of fractal dispersive fluid systems [J].Acta Geologica Sinica,2001,75(2):220～232.
[5] Deng Jun, Yang Liqiang, Zhai Yusheng.Crust-mantle interaction and dynamics of metallogenic system of Jiaodong gold ore concentrating area, China [J]. Journal of Geosciences of China, 1999, 1(1): 39～46.
[6] Deng Jun, Zhai Yusheng, Wang Jingping,et al. Shear Alteration, Mass Transfer and Gold Mineralization: An Example from Jiaodong Ore Deposit Concertrating Area, Shangdong, China [J]. Journal of China University of Geosciences, 2000, 11(3):281～287.
[7] Deng Jun, Wang Qingfei, Sun Zhongshi. Origin of gold-bearing fluid and its initiative localization mechanism in Xiadian gold deposit, Shandong province [J]. Chinese Journal of Geochemistry,2002, 21(3): 282～288.
[8] Deng Jun, Liu Wei, Sun Zhongshi, et al. Evidence of mantle rooted fluids and multi-level circulation ore-forming dynamics: A case study from the Xiadian gold deposit, Shandong province, China [J]. Science in China (Series D), 2003, 46 (Sup): 123～134.
[9] Deng Jun, Yang Liqiang, Sun Zhongshi, et al. A metallogenic model of gold deposits of the Jiaodong granite-greenstone belt [J]. Acta Geologica Sinica, 2003, 77 (4): 537～546.
[10] Deng Jun, Wang Qingfei, Wei Yanguang, et al. Metallogenic effect of transition of tectonic dynamic system [J].Journal of China University of Geosciences, 2004, 15(1): 23～28.
[11] Deng Jun, Huang Dinghua, Wang Qingfei,et al.Surplus space method: A new numerical model for prediction of shallow-seated magmatic bodies [J].Acta Geologica Sinica, 2004,78(6):1245～1249.
[12] Deng Jun, Yang Liqiang, Ge Liangsheng, et al. Research advances in the Mesozoic tectonic regimes during the formation of Jiaodong ore cluster are [J]. Progress in matural science, 2006, 16(8): 777～784.
[13] Deng J,Yang L Q,Sun Z S,et al.A metallogenic model of gold deposits of the Jiaodong granite-greenstone belt[J].Acta Geologica Sinica.2003a,77(4):537～546.
[14] Eilu P,Mikucki E J,Dugdale A L.Alteration zoning and primary geochemical dispersion at the Bronzewing lode-gold deposit,Western Australia[J].Mineralium Deposita,2001, 36:13～31.
[15] Fan H R, Zhai M G, Xie Y H,et al.Ore-forming fluids associated with granite hostedgold mineralization at the Sanshandao deposit,Jiaodong gold province,China[J]. Mineralium Deposita,2003,38:739～750.
[16] ferences from San Gabriel fault rock geochemistry and microstructures[J].J G R,100(B7),1995,13007～13020.
[17] Grant J A. The isocon diagram-a simple solution to Gresens' equation for metasomatic alteration[J].Economic Geology,1986,81:1976～1982.
[18] Gresens R L.Composition-volume relation of metasonatism[J].Chemical Geology,1967, 2:47～55.
[19] James P Evans,Frederick Mchester.Fluid-rock interaction in the San Andres system:in ferences from San Gabriel fault rock geochemistry and microstructures[J].J G R,100(B7),1995,13007～13020.
[20] John Ridley.The relations between mean rock stress and fluid flow in the crust: with reference to vein-and lode-style gold deposit[J]. Ore Deposit Review,1993:23～37.
[21] Jones M E J.Struct.Geol.,1981,3(3):333～338.
[22] Kieran D.Fluid-rock interaction in crustal shear zone:a directed percolation approach[J].Geology,1994,22:843～846.
[23] Leitch C H B,Lentz D R.The Gresens approach to mass balance constraints of alteration systems:Methods,pitfalls,examples[A].In:Lentz D R.Alteration and Alteration Process- es As-sociated with Ore-Forming Systems(Vol.11)[C].Waterloo:Geological Association of Canada,1994.161～192.
[24] MacLean W H,Kranidiotis P.Immobile elements as monitorsof mass transfer in hydroth- ermal alteration: Phelps Dodgemassive sulphide deposit,Matagami,Quebec[J].Econ- omic Geology,1987,82:951～962.
[25] MacLean W H.Mass change calculations in altered rock series[J].Mineralium Deposita, 1990,25:44～49.
[26] Maclntyer D G.Sedex-sedimentary-exhalative deposit, ore deposits,tectonics and metalogeny in the Canadian Cordillera.Ministry of Energy,Mines and Petroleum Resources, British Columbia, Queen’s Printer for British Columbia[M].Victoria: 1995: 5～20.
[27] Madeisky H E, Stanley C R.Lithogeochemical exploration ofmetasomatic zones associ- ated with volcanic-hosted massivesulfide deposits using Pearce Element Ratio analysis[J]. Inter national Geology Review,1993,35:1121～1148.
[28] Mandelbort B.B. Fractals: Form, Chance and Dimension.FreemanSan, Francisco, 1977.
[29] Mandelbort B.B. The Fractal Geometry of Nature.Freeman, San Francisco, 1982.
[30] Parry W T. Fault-fluid compositions from fluid-inclusion observations and solubilities of fracture-sealing minerals[J]. Prcambrian Research,1998,290(1～2):1～26.
[31] Sibson R H .Crustal stress, faulting and fluid flow[A].Parnell J, ed. Geological Special publications[C].Bath,The Geological Special publications House, 1994,69～84.
[32] Sibson R H.Fault rocks and fault mechanisms[J].J Geol.Soc.London,1977,133:191～213.
[33] Yang J H,Zhou X H. The Rb-Sr isochron of ore and pyrite subsamples from Linglong gold deposit,Jiaodong Peninsula,eastern China and their geological signi-ficance[J]. Chinese Sci.Bull,2000,45:2272～2276.
[34] Yang J H,Zhou X H.Rb-Sr,Sm-Nd and Pb isotope systematics of pyrite:implications for the age and genesis of lode gold deposits[J]. Geoloy,2001,29:711～714.
[35] Yang L Q,Deng J,Zhang J,et al.Preliminarystudies of Fluid Inclusions in Damoqujia Gold Deposit along Zhaoping Fault Zone,Shandong province,China[J].Acta Petrologica Sinica,2006,23(1):1～10.
[36] Zwart, H J. On the determination of polymorphic mineral associations and its application to the Bosost area (central phrenees)[J].Geol.Rundschau,1962,52:38～65.
[37] Zwart, H J. Some examples of the relations between deformation and metamorphism from the central Phrenees[J].Geol.en Mijinbouw.1963,42:143～154.
[38]岑况,钟玉芳.攀西地区基性超基性岩地球化学及嵌套韵律层的分形动力学研究[J].现代地质, 1999,13(4):408～410.
[39]陈春仔,金友渔.分形理论在成矿预测中的应用[J].矿产与地质,1997,11(4):272～275.
[40]陈光远,孙岱生,邵伟.胶东金矿成因矿物学与找矿[M].重庆出版社,1989,1～452.
[41]陈国达.成矿构造研究法.北京:地质出版社,1978.
[42]陈衍景,Pirajno F,赖勇,等.胶东矿集区大规模成矿时间和构造环境[J].岩石学报,2004,20(4):907～922.
[43]陈毓川,裴荣富,宋天锐,等.中国矿床成矿系列:第五届全国矿床会议论文集[C].北京:地质出版社,1993:89～90.
[44]陈毓川.矿床的成矿系列[J].地学前缘,1994,1(3-4):90～9.
[45]陈远荣,贾国相,徐庆鸿.元素集成快速定位预测隐伏矿的新技术研究[M].地质出版社,2003.
[46]陈远荣.有机烃气新方法寻找有色、贵金属矿床的研究:[博士学位论文].湖南长沙:中南大学,2001.
[47]成秋明.成矿过程奇异性与矿产预测定量化的新理论与新方法[J].地学前缘,2007,14(5):42～53.
[48]成秋明.非线性成矿预测理论:多重分形奇异性-广义自相似性-分形谱系模型与方法[J].地球科学-中国地质大学学报,2006,31(3):337～348.
[49]程裕琦,陈毓川,赵一鸣,等.再论矿床地成矿系列问题-兼论中生代某些矿床地成矿系列[J].地质论评,1983,29(2):127～139.
[50]寸珪,陈纪明.中华人民共和国黄金矿产图集[M].廊坊:国家黄金管理局黄金地质研究所,1992,65.
[51]邓军,张国铎,孙希贤.胶东半岛招掖金矿带控矿构造特征及灰色领域初探[J].中国区域地质,1993,(3):264～273.
[52]邓军,孙希贤.隐形类矿床的灰色特征及其灰色预测初探[C].见:何科昭主编.献给校庆四十周年文集.北京:海洋出版社,1993,217～223.
[53]邓军.山东招掖金矿带断裂构造分带与蚀变矿化分带关系研究[J].矿床地质,1994,13:17～19.
[54]邓军,徐守礼,孙希贤.模糊数学在胶东西部金矿带成矿预测研究中的应用[J].现代地质,1994, 8(2):229～235.
[55]邓军,方云,周显强.山东胶西北金矿带成矿构造应力场反演及其控矿作用[J].中国区域地质,1995,(3):252～260.
[56]邓军,方云,周显强,等.胶东半岛西北部金矿带成矿构造应力场及成矿微量元素分布特征研究[J].地球学报,1995,(1):10～21.
[57]邓军,徐守礼,吕古贤,等.胶东西北部断裂构造与成矿作用研究[J].现代地质,1996,10(4): 502～511.
[58]邓军,吕古贤,杨立强,等.构造应力场转换与界面成矿[J].地球学报,1998,19(3): 244～250.
[59]邓军,翟裕生,杨立强,等.论剪切带构造成矿系统[J].现代地质,1998,12(4): 493～500.
[60]邓军,杨立强,孙忠实,等.剪切带构造成矿动力机制与模式[J].现代地质,1999,13(2):125～129
[61]邓军,翟裕生,杨立强,等.剪切带构造-流体-成矿系统动力学模拟[J].地学前缘,1999,6(1),115～126.
[62]邓军,翟裕生,杨立强,等.构造演化与成矿系统动力学-以胶东金矿集中区为例[J].地学前缘,1999,6(2): 315～323.
[63]邓军,杨立强,方云,等.胶东地区壳-幔作用与金成矿效应[J].地质科学,2000,35(1): 60～70.
[64]邓军,杨立强,孙忠实等.构造体制转换与流体多层循环成矿动力学[J].地球科学,2000,25(4): 397～403.
[65]邓军,杨立强,方云等.成矿系统嵌套分形结构与自有序效应[J].地学前缘,2000,7(1): 133～146.
[66]邓军,杨立强,孙忠实等.矿源系统地质-地球化学例析[J].现代地质,2000,14(2): 165～172.
[67]邓军,杨立强,翟裕生,等.构造-流体-成矿系统及其动力学的理论格架与方法体系[J].地球科学,2000,25(1):71～78.
[68]邓军,方云,杨立强,等.剪切蚀变带与物质迁移及金的富集-以胶东矿集区为例[J].地球科学,2000,25(4): 428～432.
[69]邓军,孙忠实,杨立强,等.成矿流体运动系统与金质来源和富集机制讨论[J].地质科技情报,2000,19(1):41～45.
[70]邓军,王建平,王建国,等.胶东半岛西北部金矿带构造动力控矿[C].中国金都招远国际金矿地质与勘查学术论坛论文集,地震出版社,2002:55～58.
[71]邓军,王庆飞,孙忠实,等.矿物磁性与金元素富集的可能关系[J],现代地质,2002,16(2):177～179.
[72]邓军,孙忠实,候增谦,等.板块界面磁斥力形成与全球大型-超大型金矿分布规律初探[J].地质科学,2002,37(4):502～508.
[73]邓军,王庆飞,杨立强,等.胶西北金矿集区成矿作用发生的地质背景[J].地学前缘,2004, 11(4):527～533.
[74]邓军,王庆飞,黄定华.成矿流体运输物理机制研究的关键难题与方法体系[J].地球科学进展, 2004,19(3):393～398.
[75]邓军,王庆飞,杨立强,等.胶东西北部金热液成矿系统内部结构解析[J].地球科学,2005,30(1): 102～108.
[76]邓军,杨立强,葛良胜,等.胶东矿集区形成的构造体制研究进展[J].自然科学进展,2006,16(5): 513～518.
[77]邓军,杨立强,王庆飞,等.胶东矿集区金成矿系统组成与演化概论[J].矿床地质,2006,25: 67～70.
[78]丁汝福,王京彬,蔡新平,等.成矿作用研究结合综合方法技术预测隐伏金矿[J].矿产与地质,17(6):669～672.
[79]丁式江,翟裕生,邓军.胶东焦家金矿蚀变岩中元素的质量迁移[J].地质与勘探,2000,36(4):28～31.
[80]都城秋惠.变质作用与变质带[M],周云生译(1979),地质出版社,1972,1～492.
[81]范永香.初论内生金属矿床矿区地质预测的主要途径[J].地球科学,1984,4:107～116.
[82]高帮飞,邓军,王庆飞,等.风化作用元素迁移与金富集机制研究-以国内外典型红土型金矿床为例[J].黄金,2006,27(5):9～12.
[83]耿文辉,敬荣中,韦龙明,等.有色金属矿山可持续发展找矿预测方法与应用[J].矿产与地质,2004,18(104):350～355.
[84]贡恰罗夫,M.A.等.变形-化学共生组合与构造-变质分带[J].国外地质科技,1996,(31):48～53.
[85]关康,罗镇宽,苗来成,等.郭家岭型花岗岩地球化学特征与金矿化的关系[J].地质找矿论丛,1997,12(4):1～8.
[86]哈本海,武际春,戴立新,等.玲珑金矿田控矿断裂-矿化特征及成矿远景展望[J].黄金(增刊),2006,27:54～57.
[87]韩润生.初论构造成矿动力学及其隐伏矿定位预测研究内容和方法[J].地质与勘探,2003,39(1):5～9.
[88]郝广成,常和平.成矿有利度分析方法在山东平邑铜石南部地区金矿综合信息成矿预测中的应用[J].山东地质,2002,18(2):16～19.
[89]洪岩,邓永高,孔庆存,等.山东招远玲珑金矿田构造控矿规律及深部成矿预测(科研报告).1987,1～48.
[90]胡世玲.山东玲珑和郭家岭岩体的同位素年龄及其地质意义[J].岩石学报,1987,(3):83～89.
[91]胡受奚,赵懿英,徐金方,等.华北地台金矿地质[M].北京:科学出版社,1997,220.
[92]姜维明,哈本海,王启梁,等.玲珑金矿田九曲-大开头矿段深部矿体定位分析[J].黄金科学技术,2004,12(4):17～21.
[93]敬荣中,鲍光淑,郭仁敏.矿山可持续发展综合物探技术方法研究[J].矿产与地质,2002,16(3):187-190.
[94]敬荣中,鲍光淑,林剑,等.一种基于数据融合的地球物理数据联合反演方法-以VES和MT为例[J].地球物理学报,2004,47(1): 143-150.
[95]敬荣中,鲍光淑,周屹.坑道综合物探方法在生产矿山中的应用[J].中南工业大学学报,2000(1):4-8.
[96]科兹洛夫斯基,E.A.科拉超深钻井(上)[M],张秋生主译(1991).地质出版社,1984,1～218.
[97]孔庆存,宋玉国,邓永高,等.玲珑金矿田矿脉深部成矿预测方法[J].地质找矿论丛,1987,2(4):77～83.
[98]孔庆存,宋玉国,邓永高,等.山东招远玲珑金矿构造控矿规律及深部成矿预测[C].国际金矿地质与勘探学术会议论文集:东北工学院出版社,1989,385～388.
[99]李东旭,周济元.地质力学导论[M].地质出版社,1986,1～343.
[100]李洪玉,姜振富.玲珑金矿田双顶矿段地质特征及金的富集规律[J].黄金,1999,20(11):9～11.
[101]李厚民,毛景文,沈远超,等.胶西北东季金矿床钾长石和石英的Ar-Ar年龄及其意义[J].矿床地质,2003,22(1):72～77.
[102]李华芹.刘家齐,魏琳.热液矿床流体包裹体年代学研究及其地质应用[M].北京:地质出版社,1993. 125～126
[103]李俊建,罗镇宽,刘晓阳,等.玲珑金矿区成矿后花岗斑岩脉的锆石SHRIMP U-Pb年龄对胶北地体演化的制约[J].2005,12(2):317～323.
[104]李士先,刘连生.山东胶西北S型构造及其对金矿的控制作用[J].地质力学文集,1981,5:38～57.
[105]李树勋,刘喜山.韧性剪切变质带特征及与金矿化的关系[J].1988,(5):19～21.
[106]李四光.关于地质构造的三个基本概念[J].地质学报,1953,33(4):233～260.
[107]李荫清,芮宗瑶,程莱仙.玉龙斑岩铜(钼)矿床的流体包裹体及成矿作用研究[J].地质学报,1981,55(3):216～231.
[108]李兆龙,杨敏之.胶东金矿床地质地球化学[M].天津科学技术出版社,1993,1～292.
[109]林文蔚,殷秀兰.成矿流体的浓缩作用及浓缩方式研究[J].地球学报,1998,19(2): 158～165.
[110]林文蔚,殷秀兰.胶东金矿成矿流体同位素的地质特征[J].岩石矿物学杂志,1998,17(3):249～259.
[111]刘瑞珣.显微构造地质学[M].北京大学出版社,1988,1～235.
[112]刘石年.山东玲珑式金矿床矿体空间定位形式及其形成机制的探讨[J].地球科学,1884,(4):47～56
[113]刘志刚.玲珑金矿田控矿构造研究[J].长春地质学院学报,1983,(3):47～54.
[114]卢焕章,Guy Arcambault,李院生,等.山东玲珑一焦家地区形变类型与金矿的关系[J].地质学报,1999,73(2):174～190.
[115]卢焕章,J Guha,方根保.山东玲珑金矿的成矿流体特征[J].地球化学,1999,28(5):421～437.
[116]卢焕章,袁万春,张国平,等.玲珑—焦家地区主要金矿床稳定同位素及同位素年代学[J].桂林工学院学报,1999,19(1):1～8.
[117]吕古贤,邓军,郭涛,等.玲珑-焦家式金矿构造变形岩相形迹大比例尺填图与构造成矿研究[J].地球学报,1998,19(2):177～186.
[118]吕古贤,郭涛,刘杜鹃.玲珑-焦家式金矿构造地质特征及成矿构造物理化学参量因子分析-以阜山金矿区为例[J].地球学报,2002,23(5):409～416.
[119]吕古贤,郭涛,舒斌,等.构造变形岩相形迹的大比例尺填图及其对隐伏矿床地质预测-以胶东玲珑-焦家式金矿为例[J].中国区域地质,2001,20(3):313～321.
[120]吕古贤,郭涛.阜山金矿区构造变形岩相特征与成矿流体构造物理化学特征研究[J].矿床地质(增刊),1998,(17):939～942.
[121]吕古贤,侯成桥,郭涛,等.玲珑金矿田深部资源第二富集带的预测研究[J].黄金(增刊),2006,27:47～53.
[122]吕古贤,孔庆存,邓军,等.山东玲珑和焦家金矿成矿深度研究与测算[J].地质论评,1996,42(6): 550～559.
[123]吕古贤,孔庆存.胶东玲珑-焦家式金矿地质[M].北京:科学出版社,1993,1～253.
[124]吕古贤,李晓波,倪师军,等.构造物理化学研究的一个重要问题-“构造附加静水压力”及其应用[J].华南地质与矿产,1998,56(4):1～13.
[125]吕古贤,林文蔚,郭涛,等.金矿成矿过程中构造应力场转变与热液浓缩-稀释作用[J].地学前缘,2001,8(4):253～264.
[126]吕古贤,林文蔚,罗元华,等.构造物理化学与金矿成矿预测[M],北京:地质出版社,1999,1～458.
[127]吕古贤,刘瑞珣,王方正,等.成岩成矿深度构造校正测算和实测[J].地质力学学报,2000,6(3): 50～62.
[128]吕古贤,刘瑞珣,王方正,等.成岩成矿深度构造校正测算和实例[J].地质力学学报,2000,6(3):50～62.
[129]吕古贤,刘瑞珣.重力和构造力在地壳中的作用.高校地质学报,1996,2(1):28～37.
[130]吕古贤、邓军、郭涛,等.玲珑-焦家式金矿构造变形岩相形迹大比例尺填图与构造成矿研究[J].地球学报,1998,19(2):177～186.
[131]吕古贤.构造物理化学的研究与应用[J].中国地质,1997,10:45～48.
[132]吕古贤.构造物理化学基本问题与金矿成矿预测[J].地球学报,1998,19(2):117～125.
[133]吕古贤.关于构造物理化学的初步探讨[J].中国区域地质,1991,(3):254-261.
[134]吕古贤.关于构造作用力影响“静水压力”问题[J].科学通报,1995,40(3):286.
[135]吕古贤.胶东半岛构造-岩相形式及玲珑-焦家式金矿的构造动力成岩成矿地质特征研究[J].中国地质科学院院报,1991,23:23～42.
[136]吕古贤.胶东半岛构造-岩相型式及玲珑-焦家式金矿的构造动力成岩成矿地质特征研究[J].中国地质科学院院报,1991b,(23):65～80.
[137]吕古贤.胶东玲珑-焦家式金矿床矿源岩系系列研究[J].矿床地质,1998,17:935～938.
[138]吕古贤.山东玲珑金矿田和焦家金矿田成矿深度的测算与研究方法[J].中国科学(D辑),1997, 27(4):337～342.
[139]吕古贤.山东省玲珑金矿田成矿深度的研究与测算[J].科学通报,1995,40(15): 1399～1402.
[140]罗镇宽,苗来成.胶东招莱地区花岗岩和金矿床[M].冶金工业出版社,2002,1～143.
[141]骆万成,伍勤生.应用蚀变矿物测定胶东金矿的成矿年龄[J].科学通报,1987,33:(6):1245～1248.
[142]马丽芳(主编).中国地质图集[M].北京:地质出版社,2002,348.
[143]马托埃,W.地壳变形[M],孙坦,张道安译(1984).地质出版社,1980,1～339.
[144]苗来成,罗镇宽,黄佳展,等.山东招掖金矿带内花岗岩类侵入锆石SHRIMP研究及其意义.中国科学, D辑,1997,27(3): 207～213.
[145]帕塔拉哈,E. U.构造相分析,产生与发展[J].国外地质科技,1987,(5).
[146]钱建平.构造动力成矿理论若干问题的探讨[J].地质地球化学,2002,30(4):1～6.
[147]裘有守,王孔海,催克英,等.山东牟平-乳山地区变质岩和花岗岩含金性及其与金矿成矿关系-中国金矿主要类型区域成矿条件文集(胶东地区)[M].地质出版社,1988,120～174.
[148]裘有守,王孔海,杨广华,等.山东招远-掖县地区金矿区域成矿条件[M].辽宁科学技术出版社,1988,1～291.
[149]申维.分形混沌与矿产预测[M].北京:地质出版社,2002.
[150]申玉科.胶西北金矿集中区构造-蚀变网络研究:[博士学位论文].北京:中国地质大学(北京),2006:1～101.
[151]孙国胜,李绪俊,姚凤良,等.玲珑金矿田矿物组合与地球化学分带及矿体定位预测意义[J].地质与勘探,2002,38(4):28～32.
[152]孙国胜,姚凤良,胡瑞忠,等.玲珑金矿田矿体富集规律及其控制因素[J].大地构造与成矿学,2001,25(4):464～470.
[153]孙景运.胶东玲珑金矿田52号脉群成矿规律及其找矿应用[J].地质地球化学,1985,(1):71～73.
[154]孙景运,周炳煌,王金城,等.山东玲珑金矿田东山矿床构造控矿规律及其在找矿勘探上的应用[C].国际金矿地质与勘探学术会议论文集,东北工学院出版社,134～135.
[155]孙启祯.边缘成矿与成矿预测[C]∥陈毓川,主编.当代地质矿产资源勘查评价的理论与方法.北京:地震出版社,1999:26～33.
[156]万丽,王庆飞,高帮飞,等.成矿预测数据统计方法[J].现代地质,2005,19(4):615～620.
[157]万丽,王庆飞,高帮飞.成矿预测中的非线性数学方法[J].地质找矿论丛,2006,21(1):45～48.
[158]汪劲草,王国富,汤静如.玲珑-焦家地区金矿成矿构造体制的新认识[J].桂林工学院学报,2002,22(1):1～4.
[159]王鹤年,汪耀,陈延安.胶东中元古代玲珑花岗岩及其后期叠加改造作用的地质、地球化学证据[J].南京大学学报(地球科学版),(1):105～118.
[160]王继伦,李善芳,齐文秀.中国金矿物探、化探方法技术的研究与应用[M].北京:地质出版社,1997.
[161]王林祥.沂沐断裂带内构造体系特征及其复合现象[J].长春地质学院学报,1987,17(1):11～20.
[162]王明志,李闫华,鄢云飞,等.若干成矿预测理论研究综述[J].资源环境与工程,2007,21(4):363～369.
[163]王仁铎,杨明国.地质现象分形统计学研究的若干问题[J].现代地质,1998,12 (1):91～98.
[164]王秀璋,程景平.我国某些层控矿床的成矿时差和时控特征-地球化学文集[M].科学出版社,1986,14～20.
[165]王中刚,于学元,赵振华,等.稀土元素地球化学[M],科学出版社,1989,76～94
[166]韦龙明,吴烈善,李惠,等.若干类型金矿找矿方法评述与综合找矿模型[J].桂林工学院学报,2003,23(1):5～9.
[167]吴烈善,韦龙明.有机烃新方法在金矿床快速定位预测中的应用:以陕西八卦庙特大型金矿床为例[J].地球化学,2001,30(6):579～584.
[168]谢尔曼,С.И.地壳断裂发育的物理规律[M],高中和译(1980).地震出版社,1977,,1～209.
[169]徐金方.玲珑复式花岗岩基的构成及其形成时代[J].岩石学报,1991,(2):43～49.
[170]杨进辉,周新华.胶东地区玲珑金矿矿石和载金矿物Rb-Sr等时线年龄与成矿时代[J].科学通报,2000,45(14):1547～1552.
[171]杨开庆.关于构造控岩控矿与构造成岩成矿问题[J].地质力学论丛,北京:科学出版社,1982,(6):9～19.
[172]杨敏之,李治平.胶东东部金青顶金矿床围岩蚀变的地球化学、形成机理及找矿方向[J].地质找矿论丛,1989,4(2):1～17.
[173]杨敏之,吕古贤.胶东绿岩带金矿地质地球化学[M].北京:地质出版社,1996.1～221.
[174]杨敏之.金矿床围岩蚀变带地球化学-以胶东为例[M].北京:地质出版社,1998,1～120.
[175]杨士望.论胶东半岛西北部胶东群地层、金的矿源层和金矿床的层控性质[J].地质找矿论丛,1986,1(2):1～12.
[176]杨士望.论胶东半岛西北部胶东群地层、金的矿源层和金矿床的层控性质[J].地质找矿论丛,1986,1(3):39～48.
[177]杨世瑜,钟昆明.北衙斑岩型金矿床快速定位预测-影像线环结构-构造地球化学集成成矿预测方法[J].中国工程科学(增刊),2005,7:224～227.
[178]杨新岳,谢国源,李志纯.变形过程中的流体—岩石作用和变形岩石质量平衡[J].中国科学(B辑),1995,25(3):329～336.
[179]杨岳衡,刘铁兵,李厚民.多元素X射线荧光分析方法在山东郭城金矿成矿预测中的应用[J].黄金科学技术,2000,8(5):13～19.
[180]杨忠芳,徐景奎,赵伦山,等.胶东两大成因系列金矿石英包裹体氮氧同位素及成矿流体组分地球化学研究[J].矿物学报,1991,11(4):363～369.
[181]姚凤良,刘连登,孔庆存,等.胶东西北部脉状金矿[M].吉林科学技术出版社,1990,1～234.
[182]翟裕生,邓军,李晓波,等.区域成矿学[M].北京:地质出版社,1999:154～171.
[183]翟裕生,彭润民,邓军,等.成矿系统分析与新类型矿床预测[J].地学前缘,2000,7(1):123～132.
[184]翟裕生,熊永良.关于成矿系列的结构[J].地球科学,1987,12(4):375～380.
[185]翟裕生,姚书振,等.成矿系列研究[M].武汉:中国地质大学出版社,1996:1～28.
[186]翟裕生.成矿系列研究问题[J].现代地质:中国地质大学研究生院学报,1992,6(3):300～307.
[187]翟裕生.关于构造-流体-成矿作用研究的几个问题[J].地学前缘1996,3(4):230～236.
[188]翟裕生.论成矿系统[J].成矿前缘,1999,6(1):13～27.
[189]战传富.郊庐断裂带强震活动的深部构造标志[J].地震地质,1983,5(1):42～52.
[190]张德宏,张庆禧.玲珑金矿田岩石地球化学测量及其找矿效果[J].山东地质,1998,14(1):47～52.
[191]张均,周乔伟.分形方法在金矿化时空结构分析中的应用[J].现代地质,2000,14(1):56～60.
[192]张可清,杨勇.蚀变岩质量平衡计算方法介绍[J].地质科技情报,2002,21(3):104～107.
[193]张理刚.稳定同位素在地质科学中的应用[M].陕西科学技术出版社,1985,1～267.
[194]张儒瑗,从柏林.矿物温度计和矿物压力计[M].地质出版社,1983.
[195]张生,李统锦,陈义兵.长坑矿床矿化过程中元素的质量迁移及金银关系[J].地质找矿论丛,1997,12(3):33～40.
[196]张渊,王微,王威.玲珑金矿田矿石学研究[J].世界地质,1995,14(3):39～42
[197]张远飞,吴健生.基于遥感图像提取矿化蚀变信息[J].有色金属矿产与勘查,1999,8(6): 604～606.
[198]张振海,张景鑫,叶素芝.胶东金矿同位素年龄厘定[M].北京地质出版社,1994.
[199]张振海.胶东招-掖金矿带等时线的研究及测定[J].贵金属地质,1993,2(1):26～33.
[200]赵鹏大.“三联式”资源定量预测与评价[J].地球科学,2002,27(5):482～489.
[201]赵希溦.矿物中包裹体的显微镜下研究及其在地质研究中的作用[J].长春地质学院学报,1981,(4):38～46.
[202]赵震宇,王世称,许亚明,等.综合信息矿产预测理论在危机矿山资源预测中的应用思考[J].世界地质,2000,21(3):283～286.
[203]钟增球,游振东.剪切带的成分变异及体积亏损-以河台剪切带为例[J].科学通报,1995,40(10):913～916.
[204]周凤英,李兆麟.胶东台上金矿床矿物中包裹体研究[J].矿物学报,1991,11(4):403～413.
[205]周国发,吕古贤,申玉科,等.山东大庄子金矿Ⅰ号脉构造蚀变带特征及其地质意义[J].黄金,2008,29(12):7～10.
[206]周奇明,赵友方,黄华鸾,等.电吸附法寻找隐伏矿床的试验研究[J].地质与勘探,2001,(2)69～73.
[207]朱奉三.混合岩化热液型金矿床成矿作用初步研究-以招掖地区的金矿床为例[J].地质与勘探,1980,7:1～9.
[208]朱裕生,梅燕雄.成矿模式研究的几个问题[J].地球学报,1995,2:182～18.
[209]朱作山,任英忱.应用数理统计方法研究玲珑、焦家两种类型金矿床的成因[J].地质找矿论丛,1988,3(3):72～78.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |