准噶尔盆地二叠纪盆地属性的再认识及其构造意义
|
摘要
准噶尔盆地及其邻区野外剖面、钻井剖面的系统对比和地震剖面的精细解释表明,二叠系沉积演化、断裂控制沉积、箕状断-超反射特征及大地构造背景均显示,二叠纪准噶尔盆地是形成于张性背景下的断陷-裂陷盆地。准噶尔盆地及邻区火山岩地化特征、年代学数据及区域构造研究成果也证明,二叠纪是张性的大地构造背景。早二叠世—中二叠世早期以发育冲积扇沉积为特征,各构造部位的沉积环境差异较大,强烈断陷并逐渐形成坳隆相间的沉积格局,为断陷盆地的裂陷期;中二叠统中晚期由早二叠世隆坳分割的局面逐渐转化为统一的大型内陆湖盆,吐哈盆地与准噶尔盆地水体相通,形成统一的沉积体系,为断陷盆地扩张期;晚二叠世时期以出现冲积-河流相红色粗碎屑沉积为特征,准噶尔盆地和吐哈盆地分割自成沉积体系,是断陷盆地的萎缩期。因此,中生代盆地演化是建立在二叠纪张性背景的基础之上,二叠纪断陷-裂陷盆地的提出对重新认识中生代盆地演化历程将具有重要启示意义,也将对今后的油气勘探具有重要指导意义,值得进一步研究。
By making full use of field sections,drilling well sections,and seismic sections in the Junggar basin and adjacent areas,northwest China,we have studied the Permian sedimentary evolution,faults,and characteristics of seismic reflection profiles in detail.The Permian sedimentary record,fault-controlled sedimentation,and half graben-structures revealed in the seismic profiles,show that the Junggar basin is a fault-controlled depression that was formed during an extensional tectonic regime in the Permian.This conclusion is confirmed by the recent geochemical and chronologic evidence from volcanic rocks.The first evolutionary stage of the basin spans the period from the Early Permian to the early Middle Permian.This period was characterized by faulting and sediments deposited in alluvial fans.This period also led to the formation of a basin pattern characterized by alternating depressions and uplifts.An extensional stage followed during the middle to late stages of the Middle Permian,which was characterized by widespread sedimentary lacustrine facies.Similar sedimentary successions and geodynamic characteristics in the Turpan-Hami basin suggest that it and the Junggar probably formed as a single basin.The appearance of coarse clastic sediments of alluvial fan-fluvial facies in the Late Permian heralded a compression stage in the evolution of the basins,when different sedimentary successions in the two basins suggest that the Junggar and Turpan-Hami basins became separated.This new view of the Permian Junggar basin is different from previous models of foreland basin accepted by most geologists.Our new model provides further insights into the Mesozoic evolution of the Junggar basin and future petroleum exploration.
By making full use of field sections,drilling well sections,and seismic sections in the Junggar basin and adjacent areas,northwest China,we have studied the Permian sedimentary evolution,faults,and characteristics of seismic reflection profiles in detail.The Permian sedimentary record,fault-controlled sedimentation,and half graben-structures revealed in the seismic profiles,show that the Junggar basin is a fault-controlled depression that was formed during an extensional tectonic regime in the Permian.This conclusion is confirmed by the recent geochemical and chronologic evidence from volcanic rocks.The first evolutionary stage of the basin spans the period from the Early Permian to the early Middle Permian.This period was characterized by faulting and sediments deposited in alluvial fans.This period also led to the formation of a basin pattern characterized by alternating depressions and uplifts.An extensional stage followed during the middle to late stages of the Middle Permian,which was characterized by widespread sedimentary lacustrine facies.Similar sedimentary successions and geodynamic characteristics in the Turpan-Hami basin suggest that it and the Junggar probably formed as a single basin.The appearance of coarse clastic sediments of alluvial fan-fluvial facies in the Late Permian heralded a compression stage in the evolution of the basins,when different sedimentary successions in the two basins suggest that the Junggar and Turpan-Hami basins became separated.This new view of the Permian Junggar basin is different from previous models of foreland basin accepted by most geologists.Our new model provides further insights into the Mesozoic evolution of the Junggar basin and future petroleum exploration.
引文
[1]COLEMAN R G.Continental growth of Northwest China[J].Tectonics,1989,8(3):621-635.
[2]WINDLEY B F,ALLEN M B,ZHANG C,et al.Paleozoicaccretion and Cenozoic redeformation of the Chinese TianShan Range,Central Asia[J].Geology,1990,18:128-131.
[3]ALLEN M B,WINDLEY B F,ZHANG C.Paleozoic colli-sional tectonics and magmatism of Chinese Tian Shan,cen-tral Asia[J].Tectonophysics,1993,220:89-115.
[4]SENGOR A M C,NATALIN B A,BERTMAN V S.Evolu-tion of the Altaid tectonic collage and Paleozoic crustalgrowth in Eurasia[J].Nature,1993,364:299-307.
[5]CARROLL A R,GRAHAM S A,HENDRIX M S,et al.Late Paleozoic tectonic amalgamation of Northwestern Chi-na:Sedimentary record of the northern Tarim,northwesternTurpan,and southern Junggar basins[J].Geological societyof America bulletin,1995,107:571-594.
[6]GAO J,LIM,XIAO X,et al.Paleozoic tectonic evolution ofthe Tianshan orogen,northwestern China[J].Tectonophys-ics,1998,287:213-231.
[7]ZHANG Z C,GUO Z J,LIU S W.Age and tectonic signifi-cance of the mafic dyke swarm in the Kuruktag region,Xin-jiang[J].Acta Geologica Sinica,1998,72(1):29-36.
[8]WATSON M P,HAYWARD A B,PARKINSON D N,et al.Plate tectonic history,basin development and petroleumsource rock deposition onshore China[J].Marine and Petro-leum Geology,1987,4:205-225.
[9]HENDRIX M S,GRAHAM S A,CARROLL A R,et al.Sedimentary record and climatic implications of recurrent de-formation in the Tianshan:Evidence from Mesozoic strata ofthe north Tarim,South Junggar,and Turpan basins,north-west China[J].Geological Society of America Bulletin,1992,104:53-79.
[10]YIN A,NIE S,CRAIG P,et al.Late Cenozoic tectonic evo-lution of the southern Chinese Tian Shan[J].Tectonics,1998,17:1-27.
[11]SOBEL E R.Basin analysis of the Jurassic-Lower Cretaceoussouthwest Tarim basin,northwest China[J].GSA Bulletin,1999,111(5):709-724.
[12]DUMITRU T A,ZHOU D,CHANG E Z,et al.Uplift ex-humation,and deformation in Chinese Tian Shan[M]//HENDRIX.Paleozoic and Mesozoic tectonic evolution ofcentral Asia:from continental assembly to intracontinentaldeformation.Geological Society of America Memoir 194,2001:71-99.
[13]XIAO Xuchang,TANG Yaoqing,FENG Yimin,et al.Tec-tonic evolution of northern XinJiang and its adjacent regions[M].Beijing:Geological Publishing House,1992:1-169(in Chinese).
[14]HE Guoqi,LI Maosong,LIU Dequan,et al.Paleozoic crustalevolution and mineralization in Xinjiang of China[M].Uru-mqi:People s Press of Xinjiang;Hongkong:Hongkong cul-ture and education Press,1994:1-437(in Chinese).
[15]LI Jinyi.Main characteristics and emplacement processes ofthe East Junggar Ophiolites,Xinjiang China[J].Acta Petro-logica Sinica,1995,11(Suppl):73-84(in Chinese).
[16]GUO Zhaojie,MA Ruishi,WANG Chao.The Takezaly-Yi-wu ophiolitic melange zone and its tectonic setting in EastXinjiang[J].Acta of Nanjing University:Earth Science Edi-tion,1993,5(1):82-88(in Chinese).
[17]LIU Hefu,LIANG Huishe,CAI Liguo,et al.Evolution andstructural style of Tianshan and adjacent basins,Northwest-ern China[J].Earth Science—Journal of China University ofGeosciences,1994,19(6):727-741(in Chinese).
[18]LIU Hefu,WANG Zecheng,XIONG Baoxian,et al.Cou-pling analysis of Mesozoic-Cenozoic foreland basin and moun-tain system in central and western China[J].Earth ScienceFrontiers,2000,7(3):55-72(in Chinese).
[19]CAI Zhongxian,CHEN Fajing,JIA Zhenyuan.Types andtectonic evolution of Junggar Basin[J].Earth Science Fron-tiers,2000,7(4):431-440(in Chinese).
[20]CHEN Shuping,ZHANG Yiwei,TANG Liangjie,et al.Tec-tonic evolution of the Junggar foreland basin in the Late Car-boniferous-Permian[J].Acta Geologica Sinica,2001,75(4):398-408.
[21]CHEN Xin,LU Huafu,SHU Liangshu,et al.Study on tec-tonic evolution of Junggar Basin[J].Geological Journal ofChina Universities,2002,8(3):257-267(in Chinese).
[22]JIA Chengzao,WEI Guoqi,LI Benliang,et al.Tectonic evo-lution of two epochs foreland basin and its control for naturalgas accumulation in Middle-Western China[J].Acta PetroleiSinica,2003,24(2):13-27(in Chinese).
[23]WEI Yuanjiang,HE Dengfa,LEI Zhenyu,et al.Sedimentaryresponse to the activity of the Permian thrusting fault in theforeland thrust belt of the northwestern Junggar basin[J].Acta Geologica Sinica,2004,75(4):612-615(in Chinese).
[24]HE Dengfa,CHEN Xinfa,ZHANG Yijie,et al.Enrichmentcharacteristics of oil and gas in Junggar basin[J].Acta Pe-trolei Sinica,2004,25(3):1-10(in Chinese).
[25]HE Dengfa,YIN Cheng,DU Shekuan,et al.Characteristicsof structural segmentation of foreland thrust belts—a casestudy of the fault belts in the northwestern margin of Jung-gar basin[J].Earth Science Frontiers,2004,11(3):91-101(in Chinese).
[26]GRAHAM S A,HENDRIX M S,WANG L B,et al.Colli-sion successor basin of western China:impact of tectonic in-heritance on sand composition[J].Geological Society of A-merica Bulletin,1993,105:323-344.
[27]CHEN Fajing,WANG Xinwen,WANG Xinwei.Prototypetectonic evolution of Junggar basin,northwestern China[J].Earth Science Frontiers,2005,12(3):77-89(in Chinese).
[28]LI Yaohua.Natural Gas pool formation models and explora-tion direction in south Junggar basin[J].Natural Gas Indus-try,2001,21(4):27-31(in Chinese).
[29]WARTES M A,CARROLL A R,GREENE T J.Permiansedimentary record of the Turpan-Hami basin and adjacentregions,northwest China:constraints on post-amalgamationtectonic evolution[J].Geological Society of America Bulle-tin,2002,114(2):131-152.
[30]CHENG Z W,LUCAS S G.A possible GSSP for Permian-Triassic boundary[J].Albertiana,1993,12:39-44.
[31]FANG Shihu,XU Huaimin,SONG Yan,et al.Characteris-tics and evolution of the composite petroleum system in Ji-musaer sag,Eastern Junggar Basin[J].Acta GeiscienticaSinica,2005,26(3):259-264(in Chinese).
[32]ZHAO Zehui,GUO Zhaojie,ZHANG Chen,et al.Tectonicevolution of the Santanghu Basin,East Xinjiang and its im-plication for the hydrocarbon accumulation[J].Acta Scien-tiarum Naturalium Universitatis Pekinensis,2003,39(2):219-228(in Chinese).
[33]SU Weimin,LIANG Hao.The sedimentary environment ofthe Upper Permian in Santanghu basin[J].Xinjiang Petrole-um Geology,2001,22(6):497-498(in Chinese).
[34]GU Lianxing,CHU Qiang,HU Shouxi.The geologic fea-ture and genesis of the Alkali granite area of Kelamay-Haer-lyk in Xinjiang[M]//Xingjiang Geological Science,Book 2.Beijing:Geological Publishing House,1990:47-55(in Chi-nese).
[35]SONG C,JIN H.The evolution and sediment types of debrisflow and high density turbiditic current of the ShirenzigouFormation,the Lower Permian in the Sangonghe area,northpiedmont of Bogda Mountain[J].Acta Sedimentologica Sini-ca,1989,7:95-107.
[36]JIANG Z,FOWLER M G.Carotenoid-derived alkanes in oilsfrom northwestern China[J].Organic Geochemistry,1986,10:831-839.
[37]CARROLL A R,BRASSELL S C,GRAHAM S A.UpperPermian lacustrine oil shale,southern Junggar basin,NWChina[J].AAPG Bulletin,1992,76:1874-1902.
[38]CARROLL A R.Upper Permian organic facies evolution,southern Junggar basin,northwest China[J].Organic Geo-chemistry,1998,28:649-667.
[39]GREENE T J.Tectonics,basin analysis and organic geo-chemical attributes of Permian through Mesozoic depositsand their derivative oils of the Turpan-Hami basin,north-western China[D].Stanford,California:Stanford Universi-ty,2000:392.
[40]DOBRESTSOV N L,BERZIN N A,BUSLOV M M.Open-ing and tectonic evolution of the Paleo-Asian[J].Interna-tional Geology Review,1995,37:335-360.
[41]XIAO W J,WINDLEY B F,BADARCH G,et al.Palaeozo-ic accretionary and convergent tectonics of the southern Al-taids:implications for the growth of Central Asia[J].Jour-nal of the Geological Society,2004,161:339-342.
[42]XIAO W J,ZHANG L C,QIN K Z,et al.Paleozoic accre-tionary and collisional tectonics of the eastern Tianshan(China):implications for the continental growth of centralAsia[J].American Journal of Science,2004,304:370-395.
[43]CHEN Yanjing.Mineralization during collisional orogenesisand its control of the distribution of gold deposits in JunggarMountains,Xingjiang,China[J].Acta Geologica Sinica,1996,70(3):253-261(in Chinese).
[44]GU Lianxing,HU Shouxi,YU Chunshui,et al.Intrusive ac-tivities during compression-extension tectonic conversion inthe Bogda intra-continental orogen[J].Acta Petrologica Sin-ica,17(2):l87-198(in Chinese).
[45]GU Lianxing,HU Shouxi,YU Chunshui,et al.Initiation andevolution of the Bogda subduction-torn-type rift[J].ActaPetrologica Sinica,2001,17(4):585-597(in Chinese).
[46]CAO Shoulian,HE Dengfa.Evolution of the Caiwopu basin,Xinjiang[J].Geotectonica et Metallogenia.1997,21(3):262-269(in Chinese).
[47]HAN Baofu,HE Guoqi,WANG Shiguang.Postcollisionalmantle-derived magmatism and vertical growth of the conti-nental crust in north Xinjiang[J].Geological Review,1999,44(4):396-406.
[48]YARMOLYUK V V,SAMOILOV V S,IVANOV V G,etal.Compostition and sources of basalts in the late Paleozoicrift system of central Asian:geochemical and isotopic data[J].Geochemical International,1999,37(10):921-935.
[49]YANG Shufeng,CHEN Hanlin,DONG Chuanwan,et al.The discovery of Permian syenite inside Tarim basin and itsgeodynamic significance[J].Geochimica,1996,25(2):121-128(in Chinese).
[50]CHEN Hanlin,YANG Shufeng,JIA Chengzao,et al.Con-firmation of Permian intermediate-acid igneous rock zone anda new understanding of tectonic evolution in the northernpart of the Tarim basin[J].Acta Mineralogica Sinica,1998,18(3):370-376(in Chinese).
[51]ZHANG Zhicheng,GUO Zhaojie,LIU yulin,et al.Heliumand Argon isotopic compositions of mafic dyke swarm and itsimplication from Kuluketag,Xinjiang[J].Xinjiang Geology,2004,3(3):12-15(in Chinese).
[52]ALLEN M B,WINDLEY,B F,ZHANG C.Paleozoic colli-sional tectonics and magmatism of the Chinese Tien Shan,Central Asia[J].Tectonophysics,1992,220:89-115.
[53]GU Lianxing,HU Shouxi,YU Chunshui,et al.The Carbonif-erous volcanic rock and its geological setting in the Bogdaorogen,eastern Tianshan[J].Acta Petrologica Sinica,2000,16(3):305-316(in Chinese).
[54]SHU Liangshu,GUO Zhaojie,ZHU Wenbin,et al.Post col-lision tectonism and basin-range evolution in the TianshanBelt[J].Geological Journal of China Universities,2004,10(3):393-404(in Chinese).
[55]ZHOU M F,LESHER C M,YANG Z X,et al.Geochemis-try and petrogenesis of 270 Ma Ni-Cu-(PGE)sulfide-bearingmafic intrusions in the Huangshan district,Eastern Xin-jiang,Northwest China:implications for the tectonic evolu-tion of the Central Asian orogenic belt[J].Chemical Geolo-gy,2004,209:233-257.
[56]HAN B F,WANG S G,JAHN B M,et al.Depleted-mantlemagma source for the Ulungur River A-type granites fromnorth Xinjiang,China:geochemistry and Nd-Sr isotopic evi-dence,and implication for Phanerozoic crustal growth[J].Chemical Geology,1997,138:135-159.
[57]JAHN B M,WU F Y,CHEN B.Granitoids of the CentralAsian Orogenic Belt and continental growth in the Phanero-zoic[J].Trans Royal Soc Edinburgh:Earth Sci,2000,91:181-193.
[58]JAHN B M,WU F Y,CHEN B.Massive granitoid genera-tion in Central Asia:Nd isotope evidence and implication forcontinental growth in the Phanerozoic[J].Episodes,2000,23:82-92.
[59]CHEN B,JAHN B M.Geochemical and isotopic studies ofthe sedimentary and granitic rocks of the Altai orogen ofnorthwest China and their tectonic implications[J].Geolog-ical Magazine,2002,129:1-13.
[60]KOVALENKO V I,YARMOLYUK V V,KOVACH V P,et al.Sources of Phanerozoic granitoids in Central Asia:Sm-Nd isotope data[J].Geochemical International,1996,34:628-640.
[61]JAHN B M.Phanerozoic continental growth in Central Asia[J].Journal of Asian Earth Sciences,2004,23:599-603.
[62]ALLEN M B,WINDLEY B F,ZHANG C,et al.Evolutionof Turpan basin,Chinese Central Asia[J].Tectonics,1993,12:889-896.
[63]BALLY A W,CHOU I M,CLAYTON R,et al.Notes onsedimentary basins in China—report of the American sedi-mentary basins delegation to the people s Republic of China[J].U S Geological Survey,Open-Files Report,1986,108:86-327.
[64]LIU H.Geodynamic scenario and structural styles of Meso-zoic and Cenozoic basins in China[J].AAPG Bulletin,1986,70:377-395.
[65]PENG X,ZHANG G.Tectonics features of the Junggar basinand their relationship with oil and gas distribution[M]//HSU K J,ZHU X.Chinese sedimentary basins.Amster-dam:Elsevier,1989:17-31.
[66]LEI Zhenyu,BIAN Dezhi,DU Shekuan,et al.Characteris-tics of fan forming and oil-gas distribution in west-north mar-gin of Junggar basin[J].Acta Petrolei Sinica,2005,26(1):8-12(in Chinese).
[13]肖序常,汤耀庆,冯益民,等.新疆北部及其邻区大地构造[M].北京:地质出版社,1992:1-169.
[14]何国琦,李茂松,刘德权,等.中国新疆古生代地壳演化及成矿[M].乌鲁木齐:新疆人民出版社;香港:香港文化教育出版社,1994:1-437.
[15]李锦轶.新疆东准噶尔蛇绿岩的基本特征和侵位历史[J].岩石学报,1995,11(增刊):73-84.
[16]郭召杰,马瑞士,王超.新疆东部塔克扎勒—伊吾蛇绿混杂岩带及其构造背景[J].南京大学学报:地球科学版,1993,5(1):82-88.
[17]刘和甫,梁慧社,蔡立国,等.天山两侧前陆冲断系构造样式与前陆盆地演化[J].地球科学———中国地质大学学报,1994,19(6):727-741.
[18]刘和甫,汪泽成,熊保贤,等.中国西部中、新生代前陆盆地与挤压造山带耦合分析[J].地学前缘,2000,7(3):55-72.
[19]蔡忠贤,陈发景,贾振远.准噶尔盆地的类型和构造演化[J].地学前缘,2000,7(4):431-440.
[21]陈新,卢华复,舒良树,等.准噶尔盆地构造演化分析新进展[J].高校地质学报,2002,8(3):257-266.
[22]贾承造,魏国齐,李本亮,等.中国中西部两期前陆盆地的形成及其控气作用[J].石油学报,2003,24(2):13-17.
[23]蔚远江,何登发,雷振宇,等.准噶尔盆地西北缘前陆冲断带二叠纪逆冲断裂活动的沉积响应[J].地质学报,2004,75(4):612-615.
[24]何登发,陈新发,张义杰,等.准噶尔盆地油气富集规律[J].石油学报,2004,25(3):1-10.
[25]何登发,尹成,杜社宽,等.前陆冲断带构造分段特征———以准噶尔盆地西北缘断裂构造带为例[J].地学前缘,2004,11(3):91-101.
[27]陈发景,汪新文,汪新伟.准噶尔盆地的原型与构造演化[J].地学前缘,2005,12(3):77-89.
[28]李耀华.准噶尔盆地南缘天然气成藏模式及勘探方向[J].天然气工业.2001,21(4):27-31.
[31]方世虎,徐怀民,宋岩,等.准东吉木萨尔凹陷复合含油气系统特征与演化[J].地球学报,2005,26(3):259-264.
[32]赵泽辉,郭召杰,张臣,等.新疆东部三塘湖盆地构造演化及其石油地质意义[J].北京大学学报,2003,39(2):219-228.
[33]粟维民,梁浩.三塘湖盆地上二叠统芦草沟组沉积环境[J].新疆石油地质,2001,22(6):497-498.
[34]顾连兴,褚强,胡受奚.新疆克拉麦里—哈尔里克碱性花岗岩带地质特征及其成因[M]//新疆地质科学,第2辑.北京:地质出版社,1990:47-55.
[43]陈衍景.准噶尔造山带碰撞体制的成矿作用及金等矿床分布规律[J].地质学报,1996,70(3):253-261.
[44]顾连兴,胡受奚,于春水,等.博格达陆内碰撞造山带挤压-拉张构造转折期的侵入活动[J].岩石学报,2001,17(2):187-198.
[45]顾连兴,胡受奚,于春水,等.论博格达俯冲撕裂型裂谷的形成与演化[J].岩石学报,2001,17(4):585-597.
[46]曹守连,何登发.柴窝堡盆地的构造演化[J].大地构造与成矿学,1997,21(3):262-269.
[49]杨树锋,陈汉林,董传万,等.塔里木盆地二叠纪正长岩的发现及其地球动力学意义[J].地球化学,1996,25(2):121-128.
[50]陈汉林,杨树锋,贾承造,等.塔里木盆地北部二叠纪中酸性火成岩带的厘定及其对塔北构造演化的新认识[J].矿物学报,1998,18(3):370-376.
[51]张志诚,郭召杰,刘玉琳,等.新疆库鲁克塔格地区基性岩墙群氦氩同位素组成及其地质意义[J].新疆地质,2004,3(3):12-15.
[53]顾连兴,胡受奚,于春水,等.东天山博格达山造山带石炭纪火山岩及其形成地质环境[J].岩石学报,2000,16(3):305-316.
[54]舒良树,郭召杰,朱文斌,等.天山地区碰撞后构造与盆山演化[J].高校地质学报,2004,10(3):393-404.
[66]雷振宇,卞德智,杜社宽,等.准噶尔盆地西北缘扇体形成特征及油气分布规律[J].石油学报,2005,26(1):8-12.
①王昌桂,赵文智,周立发,等.新疆北部地区诸盆地二叠系综合评价及勘探目标选择成果报告.西安:西北大学地质系,1999.
②新疆维吾尔自治区地质矿产局.1∶20万地质图,乌鲁木齐幅.1965.
③新疆油田公司勘探开发研究院.新疆油田勘探开发研究院成果论文集,2001-2002.
①新疆油田公司勘探开发研究院.新疆油田勘探开发研究院成果论文集,2001-2002.
①新疆维吾尔自治区地质矿产局.新疆维吾尔自治区区域地质志.1∶100万地质图.北京:地质出版社,1993.
②刘楼军,徐怀民,等.准噶尔盆地东部外围区石油地质条件分析及早期评价.新疆石油管理局地质调查处,石油大学(华东),2000.
①王昌桂,赵文智,周立发,等.新疆北部地区诸盆地二叠系综合评价及勘探目标选择成果报告.西安:西北大学地质系,1999.
①新疆油田公司勘探开发研究院.新疆油田勘探开发研究院成果论文集,2001-2002.
①王昌桂,赵文智,周立发,等.新疆北部地区诸盆地二叠系综合评价及勘探目标选择成果报告.西安:西北大学地质系,1999.
[2]WINDLEY B F,ALLEN M B,ZHANG C,et al.Paleozoicaccretion and Cenozoic redeformation of the Chinese TianShan Range,Central Asia[J].Geology,1990,18:128-131.
[3]ALLEN M B,WINDLEY B F,ZHANG C.Paleozoic colli-sional tectonics and magmatism of Chinese Tian Shan,cen-tral Asia[J].Tectonophysics,1993,220:89-115.
[4]SENGOR A M C,NATALIN B A,BERTMAN V S.Evolu-tion of the Altaid tectonic collage and Paleozoic crustalgrowth in Eurasia[J].Nature,1993,364:299-307.
[5]CARROLL A R,GRAHAM S A,HENDRIX M S,et al.Late Paleozoic tectonic amalgamation of Northwestern Chi-na:Sedimentary record of the northern Tarim,northwesternTurpan,and southern Junggar basins[J].Geological societyof America bulletin,1995,107:571-594.
[6]GAO J,LIM,XIAO X,et al.Paleozoic tectonic evolution ofthe Tianshan orogen,northwestern China[J].Tectonophys-ics,1998,287:213-231.
[7]ZHANG Z C,GUO Z J,LIU S W.Age and tectonic signifi-cance of the mafic dyke swarm in the Kuruktag region,Xin-jiang[J].Acta Geologica Sinica,1998,72(1):29-36.
[8]WATSON M P,HAYWARD A B,PARKINSON D N,et al.Plate tectonic history,basin development and petroleumsource rock deposition onshore China[J].Marine and Petro-leum Geology,1987,4:205-225.
[9]HENDRIX M S,GRAHAM S A,CARROLL A R,et al.Sedimentary record and climatic implications of recurrent de-formation in the Tianshan:Evidence from Mesozoic strata ofthe north Tarim,South Junggar,and Turpan basins,north-west China[J].Geological Society of America Bulletin,1992,104:53-79.
[10]YIN A,NIE S,CRAIG P,et al.Late Cenozoic tectonic evo-lution of the southern Chinese Tian Shan[J].Tectonics,1998,17:1-27.
[11]SOBEL E R.Basin analysis of the Jurassic-Lower Cretaceoussouthwest Tarim basin,northwest China[J].GSA Bulletin,1999,111(5):709-724.
[12]DUMITRU T A,ZHOU D,CHANG E Z,et al.Uplift ex-humation,and deformation in Chinese Tian Shan[M]//HENDRIX.Paleozoic and Mesozoic tectonic evolution ofcentral Asia:from continental assembly to intracontinentaldeformation.Geological Society of America Memoir 194,2001:71-99.
[13]XIAO Xuchang,TANG Yaoqing,FENG Yimin,et al.Tec-tonic evolution of northern XinJiang and its adjacent regions[M].Beijing:Geological Publishing House,1992:1-169(in Chinese).
[14]HE Guoqi,LI Maosong,LIU Dequan,et al.Paleozoic crustalevolution and mineralization in Xinjiang of China[M].Uru-mqi:People s Press of Xinjiang;Hongkong:Hongkong cul-ture and education Press,1994:1-437(in Chinese).
[15]LI Jinyi.Main characteristics and emplacement processes ofthe East Junggar Ophiolites,Xinjiang China[J].Acta Petro-logica Sinica,1995,11(Suppl):73-84(in Chinese).
[16]GUO Zhaojie,MA Ruishi,WANG Chao.The Takezaly-Yi-wu ophiolitic melange zone and its tectonic setting in EastXinjiang[J].Acta of Nanjing University:Earth Science Edi-tion,1993,5(1):82-88(in Chinese).
[17]LIU Hefu,LIANG Huishe,CAI Liguo,et al.Evolution andstructural style of Tianshan and adjacent basins,Northwest-ern China[J].Earth Science—Journal of China University ofGeosciences,1994,19(6):727-741(in Chinese).
[18]LIU Hefu,WANG Zecheng,XIONG Baoxian,et al.Cou-pling analysis of Mesozoic-Cenozoic foreland basin and moun-tain system in central and western China[J].Earth ScienceFrontiers,2000,7(3):55-72(in Chinese).
[19]CAI Zhongxian,CHEN Fajing,JIA Zhenyuan.Types andtectonic evolution of Junggar Basin[J].Earth Science Fron-tiers,2000,7(4):431-440(in Chinese).
[20]CHEN Shuping,ZHANG Yiwei,TANG Liangjie,et al.Tec-tonic evolution of the Junggar foreland basin in the Late Car-boniferous-Permian[J].Acta Geologica Sinica,2001,75(4):398-408.
[21]CHEN Xin,LU Huafu,SHU Liangshu,et al.Study on tec-tonic evolution of Junggar Basin[J].Geological Journal ofChina Universities,2002,8(3):257-267(in Chinese).
[22]JIA Chengzao,WEI Guoqi,LI Benliang,et al.Tectonic evo-lution of two epochs foreland basin and its control for naturalgas accumulation in Middle-Western China[J].Acta PetroleiSinica,2003,24(2):13-27(in Chinese).
[23]WEI Yuanjiang,HE Dengfa,LEI Zhenyu,et al.Sedimentaryresponse to the activity of the Permian thrusting fault in theforeland thrust belt of the northwestern Junggar basin[J].Acta Geologica Sinica,2004,75(4):612-615(in Chinese).
[24]HE Dengfa,CHEN Xinfa,ZHANG Yijie,et al.Enrichmentcharacteristics of oil and gas in Junggar basin[J].Acta Pe-trolei Sinica,2004,25(3):1-10(in Chinese).
[25]HE Dengfa,YIN Cheng,DU Shekuan,et al.Characteristicsof structural segmentation of foreland thrust belts—a casestudy of the fault belts in the northwestern margin of Jung-gar basin[J].Earth Science Frontiers,2004,11(3):91-101(in Chinese).
[26]GRAHAM S A,HENDRIX M S,WANG L B,et al.Colli-sion successor basin of western China:impact of tectonic in-heritance on sand composition[J].Geological Society of A-merica Bulletin,1993,105:323-344.
[27]CHEN Fajing,WANG Xinwen,WANG Xinwei.Prototypetectonic evolution of Junggar basin,northwestern China[J].Earth Science Frontiers,2005,12(3):77-89(in Chinese).
[28]LI Yaohua.Natural Gas pool formation models and explora-tion direction in south Junggar basin[J].Natural Gas Indus-try,2001,21(4):27-31(in Chinese).
[29]WARTES M A,CARROLL A R,GREENE T J.Permiansedimentary record of the Turpan-Hami basin and adjacentregions,northwest China:constraints on post-amalgamationtectonic evolution[J].Geological Society of America Bulle-tin,2002,114(2):131-152.
[30]CHENG Z W,LUCAS S G.A possible GSSP for Permian-Triassic boundary[J].Albertiana,1993,12:39-44.
[31]FANG Shihu,XU Huaimin,SONG Yan,et al.Characteris-tics and evolution of the composite petroleum system in Ji-musaer sag,Eastern Junggar Basin[J].Acta GeiscienticaSinica,2005,26(3):259-264(in Chinese).
[32]ZHAO Zehui,GUO Zhaojie,ZHANG Chen,et al.Tectonicevolution of the Santanghu Basin,East Xinjiang and its im-plication for the hydrocarbon accumulation[J].Acta Scien-tiarum Naturalium Universitatis Pekinensis,2003,39(2):219-228(in Chinese).
[33]SU Weimin,LIANG Hao.The sedimentary environment ofthe Upper Permian in Santanghu basin[J].Xinjiang Petrole-um Geology,2001,22(6):497-498(in Chinese).
[34]GU Lianxing,CHU Qiang,HU Shouxi.The geologic fea-ture and genesis of the Alkali granite area of Kelamay-Haer-lyk in Xinjiang[M]//Xingjiang Geological Science,Book 2.Beijing:Geological Publishing House,1990:47-55(in Chi-nese).
[35]SONG C,JIN H.The evolution and sediment types of debrisflow and high density turbiditic current of the ShirenzigouFormation,the Lower Permian in the Sangonghe area,northpiedmont of Bogda Mountain[J].Acta Sedimentologica Sini-ca,1989,7:95-107.
[36]JIANG Z,FOWLER M G.Carotenoid-derived alkanes in oilsfrom northwestern China[J].Organic Geochemistry,1986,10:831-839.
[37]CARROLL A R,BRASSELL S C,GRAHAM S A.UpperPermian lacustrine oil shale,southern Junggar basin,NWChina[J].AAPG Bulletin,1992,76:1874-1902.
[38]CARROLL A R.Upper Permian organic facies evolution,southern Junggar basin,northwest China[J].Organic Geo-chemistry,1998,28:649-667.
[39]GREENE T J.Tectonics,basin analysis and organic geo-chemical attributes of Permian through Mesozoic depositsand their derivative oils of the Turpan-Hami basin,north-western China[D].Stanford,California:Stanford Universi-ty,2000:392.
[40]DOBRESTSOV N L,BERZIN N A,BUSLOV M M.Open-ing and tectonic evolution of the Paleo-Asian[J].Interna-tional Geology Review,1995,37:335-360.
[41]XIAO W J,WINDLEY B F,BADARCH G,et al.Palaeozo-ic accretionary and convergent tectonics of the southern Al-taids:implications for the growth of Central Asia[J].Jour-nal of the Geological Society,2004,161:339-342.
[42]XIAO W J,ZHANG L C,QIN K Z,et al.Paleozoic accre-tionary and collisional tectonics of the eastern Tianshan(China):implications for the continental growth of centralAsia[J].American Journal of Science,2004,304:370-395.
[43]CHEN Yanjing.Mineralization during collisional orogenesisand its control of the distribution of gold deposits in JunggarMountains,Xingjiang,China[J].Acta Geologica Sinica,1996,70(3):253-261(in Chinese).
[44]GU Lianxing,HU Shouxi,YU Chunshui,et al.Intrusive ac-tivities during compression-extension tectonic conversion inthe Bogda intra-continental orogen[J].Acta Petrologica Sin-ica,17(2):l87-198(in Chinese).
[45]GU Lianxing,HU Shouxi,YU Chunshui,et al.Initiation andevolution of the Bogda subduction-torn-type rift[J].ActaPetrologica Sinica,2001,17(4):585-597(in Chinese).
[46]CAO Shoulian,HE Dengfa.Evolution of the Caiwopu basin,Xinjiang[J].Geotectonica et Metallogenia.1997,21(3):262-269(in Chinese).
[47]HAN Baofu,HE Guoqi,WANG Shiguang.Postcollisionalmantle-derived magmatism and vertical growth of the conti-nental crust in north Xinjiang[J].Geological Review,1999,44(4):396-406.
[48]YARMOLYUK V V,SAMOILOV V S,IVANOV V G,etal.Compostition and sources of basalts in the late Paleozoicrift system of central Asian:geochemical and isotopic data[J].Geochemical International,1999,37(10):921-935.
[49]YANG Shufeng,CHEN Hanlin,DONG Chuanwan,et al.The discovery of Permian syenite inside Tarim basin and itsgeodynamic significance[J].Geochimica,1996,25(2):121-128(in Chinese).
[50]CHEN Hanlin,YANG Shufeng,JIA Chengzao,et al.Con-firmation of Permian intermediate-acid igneous rock zone anda new understanding of tectonic evolution in the northernpart of the Tarim basin[J].Acta Mineralogica Sinica,1998,18(3):370-376(in Chinese).
[51]ZHANG Zhicheng,GUO Zhaojie,LIU yulin,et al.Heliumand Argon isotopic compositions of mafic dyke swarm and itsimplication from Kuluketag,Xinjiang[J].Xinjiang Geology,2004,3(3):12-15(in Chinese).
[52]ALLEN M B,WINDLEY,B F,ZHANG C.Paleozoic colli-sional tectonics and magmatism of the Chinese Tien Shan,Central Asia[J].Tectonophysics,1992,220:89-115.
[53]GU Lianxing,HU Shouxi,YU Chunshui,et al.The Carbonif-erous volcanic rock and its geological setting in the Bogdaorogen,eastern Tianshan[J].Acta Petrologica Sinica,2000,16(3):305-316(in Chinese).
[54]SHU Liangshu,GUO Zhaojie,ZHU Wenbin,et al.Post col-lision tectonism and basin-range evolution in the TianshanBelt[J].Geological Journal of China Universities,2004,10(3):393-404(in Chinese).
[55]ZHOU M F,LESHER C M,YANG Z X,et al.Geochemis-try and petrogenesis of 270 Ma Ni-Cu-(PGE)sulfide-bearingmafic intrusions in the Huangshan district,Eastern Xin-jiang,Northwest China:implications for the tectonic evolu-tion of the Central Asian orogenic belt[J].Chemical Geolo-gy,2004,209:233-257.
[56]HAN B F,WANG S G,JAHN B M,et al.Depleted-mantlemagma source for the Ulungur River A-type granites fromnorth Xinjiang,China:geochemistry and Nd-Sr isotopic evi-dence,and implication for Phanerozoic crustal growth[J].Chemical Geology,1997,138:135-159.
[57]JAHN B M,WU F Y,CHEN B.Granitoids of the CentralAsian Orogenic Belt and continental growth in the Phanero-zoic[J].Trans Royal Soc Edinburgh:Earth Sci,2000,91:181-193.
[58]JAHN B M,WU F Y,CHEN B.Massive granitoid genera-tion in Central Asia:Nd isotope evidence and implication forcontinental growth in the Phanerozoic[J].Episodes,2000,23:82-92.
[59]CHEN B,JAHN B M.Geochemical and isotopic studies ofthe sedimentary and granitic rocks of the Altai orogen ofnorthwest China and their tectonic implications[J].Geolog-ical Magazine,2002,129:1-13.
[60]KOVALENKO V I,YARMOLYUK V V,KOVACH V P,et al.Sources of Phanerozoic granitoids in Central Asia:Sm-Nd isotope data[J].Geochemical International,1996,34:628-640.
[61]JAHN B M.Phanerozoic continental growth in Central Asia[J].Journal of Asian Earth Sciences,2004,23:599-603.
[62]ALLEN M B,WINDLEY B F,ZHANG C,et al.Evolutionof Turpan basin,Chinese Central Asia[J].Tectonics,1993,12:889-896.
[63]BALLY A W,CHOU I M,CLAYTON R,et al.Notes onsedimentary basins in China—report of the American sedi-mentary basins delegation to the people s Republic of China[J].U S Geological Survey,Open-Files Report,1986,108:86-327.
[64]LIU H.Geodynamic scenario and structural styles of Meso-zoic and Cenozoic basins in China[J].AAPG Bulletin,1986,70:377-395.
[65]PENG X,ZHANG G.Tectonics features of the Junggar basinand their relationship with oil and gas distribution[M]//HSU K J,ZHU X.Chinese sedimentary basins.Amster-dam:Elsevier,1989:17-31.
[66]LEI Zhenyu,BIAN Dezhi,DU Shekuan,et al.Characteris-tics of fan forming and oil-gas distribution in west-north mar-gin of Junggar basin[J].Acta Petrolei Sinica,2005,26(1):8-12(in Chinese).
[13]肖序常,汤耀庆,冯益民,等.新疆北部及其邻区大地构造[M].北京:地质出版社,1992:1-169.
[14]何国琦,李茂松,刘德权,等.中国新疆古生代地壳演化及成矿[M].乌鲁木齐:新疆人民出版社;香港:香港文化教育出版社,1994:1-437.
[15]李锦轶.新疆东准噶尔蛇绿岩的基本特征和侵位历史[J].岩石学报,1995,11(增刊):73-84.
[16]郭召杰,马瑞士,王超.新疆东部塔克扎勒—伊吾蛇绿混杂岩带及其构造背景[J].南京大学学报:地球科学版,1993,5(1):82-88.
[17]刘和甫,梁慧社,蔡立国,等.天山两侧前陆冲断系构造样式与前陆盆地演化[J].地球科学———中国地质大学学报,1994,19(6):727-741.
[18]刘和甫,汪泽成,熊保贤,等.中国西部中、新生代前陆盆地与挤压造山带耦合分析[J].地学前缘,2000,7(3):55-72.
[19]蔡忠贤,陈发景,贾振远.准噶尔盆地的类型和构造演化[J].地学前缘,2000,7(4):431-440.
[21]陈新,卢华复,舒良树,等.准噶尔盆地构造演化分析新进展[J].高校地质学报,2002,8(3):257-266.
[22]贾承造,魏国齐,李本亮,等.中国中西部两期前陆盆地的形成及其控气作用[J].石油学报,2003,24(2):13-17.
[23]蔚远江,何登发,雷振宇,等.准噶尔盆地西北缘前陆冲断带二叠纪逆冲断裂活动的沉积响应[J].地质学报,2004,75(4):612-615.
[24]何登发,陈新发,张义杰,等.准噶尔盆地油气富集规律[J].石油学报,2004,25(3):1-10.
[25]何登发,尹成,杜社宽,等.前陆冲断带构造分段特征———以准噶尔盆地西北缘断裂构造带为例[J].地学前缘,2004,11(3):91-101.
[27]陈发景,汪新文,汪新伟.准噶尔盆地的原型与构造演化[J].地学前缘,2005,12(3):77-89.
[28]李耀华.准噶尔盆地南缘天然气成藏模式及勘探方向[J].天然气工业.2001,21(4):27-31.
[31]方世虎,徐怀民,宋岩,等.准东吉木萨尔凹陷复合含油气系统特征与演化[J].地球学报,2005,26(3):259-264.
[32]赵泽辉,郭召杰,张臣,等.新疆东部三塘湖盆地构造演化及其石油地质意义[J].北京大学学报,2003,39(2):219-228.
[33]粟维民,梁浩.三塘湖盆地上二叠统芦草沟组沉积环境[J].新疆石油地质,2001,22(6):497-498.
[34]顾连兴,褚强,胡受奚.新疆克拉麦里—哈尔里克碱性花岗岩带地质特征及其成因[M]//新疆地质科学,第2辑.北京:地质出版社,1990:47-55.
[43]陈衍景.准噶尔造山带碰撞体制的成矿作用及金等矿床分布规律[J].地质学报,1996,70(3):253-261.
[44]顾连兴,胡受奚,于春水,等.博格达陆内碰撞造山带挤压-拉张构造转折期的侵入活动[J].岩石学报,2001,17(2):187-198.
[45]顾连兴,胡受奚,于春水,等.论博格达俯冲撕裂型裂谷的形成与演化[J].岩石学报,2001,17(4):585-597.
[46]曹守连,何登发.柴窝堡盆地的构造演化[J].大地构造与成矿学,1997,21(3):262-269.
[49]杨树锋,陈汉林,董传万,等.塔里木盆地二叠纪正长岩的发现及其地球动力学意义[J].地球化学,1996,25(2):121-128.
[50]陈汉林,杨树锋,贾承造,等.塔里木盆地北部二叠纪中酸性火成岩带的厘定及其对塔北构造演化的新认识[J].矿物学报,1998,18(3):370-376.
[51]张志诚,郭召杰,刘玉琳,等.新疆库鲁克塔格地区基性岩墙群氦氩同位素组成及其地质意义[J].新疆地质,2004,3(3):12-15.
[53]顾连兴,胡受奚,于春水,等.东天山博格达山造山带石炭纪火山岩及其形成地质环境[J].岩石学报,2000,16(3):305-316.
[54]舒良树,郭召杰,朱文斌,等.天山地区碰撞后构造与盆山演化[J].高校地质学报,2004,10(3):393-404.
[66]雷振宇,卞德智,杜社宽,等.准噶尔盆地西北缘扇体形成特征及油气分布规律[J].石油学报,2005,26(1):8-12.
①王昌桂,赵文智,周立发,等.新疆北部地区诸盆地二叠系综合评价及勘探目标选择成果报告.西安:西北大学地质系,1999.
②新疆维吾尔自治区地质矿产局.1∶20万地质图,乌鲁木齐幅.1965.
③新疆油田公司勘探开发研究院.新疆油田勘探开发研究院成果论文集,2001-2002.
①新疆油田公司勘探开发研究院.新疆油田勘探开发研究院成果论文集,2001-2002.
①新疆维吾尔自治区地质矿产局.新疆维吾尔自治区区域地质志.1∶100万地质图.北京:地质出版社,1993.
②刘楼军,徐怀民,等.准噶尔盆地东部外围区石油地质条件分析及早期评价.新疆石油管理局地质调查处,石油大学(华东),2000.
①王昌桂,赵文智,周立发,等.新疆北部地区诸盆地二叠系综合评价及勘探目标选择成果报告.西安:西北大学地质系,1999.
①新疆油田公司勘探开发研究院.新疆油田勘探开发研究院成果论文集,2001-2002.
①王昌桂,赵文智,周立发,等.新疆北部地区诸盆地二叠系综合评价及勘探目标选择成果报告.西安:西北大学地质系,1999.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心