[1] GUO Zhaojie,YIN An,ROBINSON A,et al.Geochronology and geochemistry of deep-drill-core samples from the basement of the central Tarim Basin[J].Journal of Asian Earth Sciences,2005,25(1):45-56.
[2] XU Zhiqin,HE Bizhu,ZHANG Chuanlin,et al.Tectonic framework and crustal evolution of the Precambrian basement of the Tarim Block in NW China:new geochronological evidence from deep drilling samples[J].Precambrian Research,2013,235:150-162.
[3] 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[M].北京:地质出版社,1993:1-841.
Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomous Region.Regional geology of Xinjiang Uygur Autonomous Region[M].Beijing:Geological Publishing House,1993:1-841.
[4] 贾承造,张师本,吴绍祖.塔里木盆地及周边地层[M].北京:科学出版社,2004:1-19.
JIA Chengzao,ZHANG Shiben,WU Shaozu.Stratigraphy of the Tarim Basin and adjacent areas[M].Beijing:Science Press,2004:1-19.
[5] XU Bei,ZOU Haibo,CHEN Yan,et al.The Sugetbrak basalts from northwestern Tarim Block of northwest China:geochronology,geochemistry and implications for Rodinia breakup and ice age in the Late Neoproterozoic[J].Precambrian Research,2013,236:214-226.
[6] GE Rongfeng,ZHU Wenbin,ZHENG Bihai,et al.Early Pan-African magmatism in the Tarim Craton:insights from zircon U-Pb-Lu-Hf isotope and geochemistry of granitoids in the Korla area,NW China[J].Precambrian Research,2012,212/213:117-138.
[7] GE Rongfeng,ZHU Wenbin,WILDE S A,et al.Neoproterozoic to Paleozoic long-lived accretionary orogeny in the northern Tarim Craton[J].Tectonics,2014,33(3):302-329.
[8] TURNER S A.Sedimentary record of Late Neoproterozoic rifting in the NW Tarim Basin,China[J].Precambrian Research,2010,181(1/4):85-96.
[9] GAO Jun,WANG Xinshui,KLEMD R,et al.Record of assembly and breakup of Rodinia in the Southwestern Altaids:evidence from Neoproterozoic magmatism in the Chinese Western Tianshan Orogen[J].Journal of Asian Earth Sciences,2015,113 (Part 1):173-193.
[10] 潘文庆,陈永权,熊益学,等.塔里木盆地下寒武统烃源岩沉积相研究及其油气勘探指导意义[J].天然气地球科学,2015,26(7):1224-1232.
PAN Wenqing,CHEN Yongquan,XIONG Yixue,et al.Sedimentary facies research and implications to advantaged exploration regions on lower Cambrian source rocks,Tarim Basin[J].Natural Gas Geoscience,2015,26(7):1224-1232.
[11] 杜金虎,潘文庆.塔里木盆地寒武系盐下白云岩油气成藏条件与勘探方向[J].石油勘探与开发,2016,43(3):327-339.
DU Jinhu,PAN Wenqing.Accumulation conditions and play targets of oil and gas in the Cambrian subsalt dolomite,Tarim Basin,NW China[J].Petroleum Exploration and Development,2016,43(3):327-339.
[12] 管树巍,吴林,任荣,等.中国主要克拉通前寒武纪裂谷分布与油气勘探前景[J].石油学报,2017,38(1):9-22.
GUAN Shuwei,WU Lin,REN Rong,et al.Distribution and petroleum prospect of Precambrian rifts in the main cratons,China[J].Acta Petrolei Sinica,2017,38(1):9-22.
[13] LU Songnian,LI Huaikun,ZHANG Chuanlin,et al.Geological and geochronological evidence for the Precambrian evolution of the Tarim Craton and surrounding continental fragments[J].Precambrian Research,2008,160(1/2):94-107.
[14] LI Z X,BOGDANOVA S V,COLLINS A S,et al.Assembly,configuration,and break-up history of Rodinia:a synthesis[J].Precambrian Research,2008,160(1/2):179-210.
[15] LI Zhengxiang,EVANS D A D,HALVERSON G P.Neoproterozoic glaciations in a revised global palaeogeography from the breakup of Rodinia to the assembly of Gondwanaland[J].Sedimentary Geology,2013,294:219-232.
[16] 冯本智,周裕文,迟仕福,等.新疆库鲁克塔格地区前震旦纪地质与贵重、有色金属矿床[M].北京:地质出版社,1995:1-29.
FENG Benzhi,ZHOU Yuwen,CHI Shifu,et al.Presinian geology,precious and non-ferrous metal deposits in Kuruktag area,Xinjiang uygur autonomous region,China[M].Beijing:Geological Publishing House,1995:1-29.
[17] 黄智斌,王振华,杨芝林,等.库鲁克塔格地区石油地质综合研究及库车地区野外地质考察基地建设:上卷[R].库尔勒:塔里木油田公司勘探开发研究院,2009:1-545.
HUANG Zhibin,WANG Zhenhua,YANG Zhilin,et al.Comprehensive study on petroleum geology in Kuruktag area and base construction of field geology investigation in Kuqa area:first volume[R].Korla:Research Institute of Petroleum Exploration & Development of Tarim Oilfield Company,2009:1-545.
[18] LONG Xiaoping,YUAN Chao,SUN Min,et al.Reworking of the Tarim Craton by underplating of mantle plume-derived magmas:evidence from Neoproterozoic granitoids in the Kuluketage area,NW China[J].Precambrian Research,2011,187(1/2):1-14.
[19] XU Bei,XIAO Shuhai,ZOU Haibo,et al.SHRIMP zircon U-Pb age constraints on Neoproterozoic Quruqtagh diamictites in NW China[J].Precambrian Research,2009,168(3/4):247-258.
[20] HE Jingwen,ZHU Wenbin,GE Rongfeng.New age constraints on Neoproterozoic diamicites in Kuruktag,NW China and Precambrian crustal evolution of the Tarim Craton[J].Precambrian Research,2014,241:44-60.
[21] BIALAS R W,BUCK W R,QIN Ran.How much magma is required to rift a continent[J].Earth and Planetary Science Letters,2010,292(1/2):68-78.
[22] WANG Jian,LI Zhengxiang.History of Neoproterozoic rift basins in South China:implications for Rodinia break-up[J].Precambrian Research,2003,122(1/4):141-158.
[23] ZHANG Chuanlin,LI Zhengxiang,LI Xianhua,et al.Neoproterozoic bimodal intrusive complex in the southwestern Tarim block,Northwest China:age,geochemistry,and implications for the rifting of Rodinia[J].International Geology Review,2006,48(2):112-128.
[24] ZHANG Chuanlin,YANG Dongsheng,WANG Hongyan,et al.Neoproterozoic mafic dykes and basalts in the southern margin of Tarim,Northwest China:age,geochemistry and geodynamic implications[J].Acta Geologica Sinica,2010,84(3):549-562.
[25] ZHANG Chuanlin,YE Xiantao,ZOU Haibo,et al.Neoproterozoic sedimentary basin evolution in southwestern Tarim,NW China:new evidence from field observations,detrital zircon U-Pb ages and Hf isotope compositions[J].Precambrian Research,2016,280:31-45.
[26] ZHANG Chuanlin,LI Zhengxiang,LI Xianhua,et al.Neoproterozoic mafic dyke swarms at the northern margin of the Tarim Block,NW China:age,geochemistry,petrogenesis and tectonic implications[J].Journal of Asian Earth Sciences,2009,35(2):167-179.
[27] HE Jingwen,ZHU Wenbin,GE Rongfeng,et al.Detrital zircon U-Pb ages and Hf isotopes of Neoproterozoic strata in the Aksu area,northwestern Tarim Craton:implications for supercontinent reconstruction and crustal evolution[J].Precambrian Research,2014,254:194-209.
[28] ZHAO P,CHEN Y,ZHAN S,et al.The apparent polar wander path of the Tarim block (NW China) since the Neoproterozoic and its implications for a long-term Tarim-Australia connection[J].Precambrian Research,2014,242:39-57.
[29] 张英利,王宗起,闫臻,等.库鲁克塔格地区新元古代贝义西组的构造环境:来自碎屑岩地球化学的证据[J].岩石学报 ,2011,27(6):1785-1796.
ZHANG Yingli,WANG Zongqi,YAN Zhen,et al.Tectonic setting of Neoproterozoic Beiyixi Formation in Quruqtagh area,Xinjiang:evidence from geochemistry of clastic rocks[J].Acta Petrologica Sinica,2011,27(6):1785-1796.
[30] XU Bei,JIAN Ping,ZHENG Haifei,et al.U-Pb zircon geochronology and geochemistry of Neoproterozoic volcanic rocks in the Tarim Block of northwest China:implications for the breakup of Rodinia supercontinent and Neoproterozoic glaciations[J].Precambrian Research,2005,136(2):107-123.
[31] 姜常义,白开寅,黑爱芝,等.库鲁克塔格地区火山岩的岩浆过程与源区组成[J].岩石矿物学杂志,2000,19(1):8-18.
JIANG Changyi,BAI Kaiyin,HEI Aizhi,et al.Petrology,geochemistry,magmatic process and source composition of Sinian-Cambrian volcanic rocks in Kuruktag area[J].Acta Petrologica et Mineralogica,2000,19(1):8-18.
[32] 展新忠,陈川,张晓帆.新疆库鲁克塔格南华纪火山岩地球化学特征及其意义[J].新疆大学学报: 自然科学版,2013,30(3):354-360.
ZHAN Xinzhong,CHEN Chuan,ZHANG Xiaofan.Geology-geochemistry characteristics and its significance of the Nanhua volcanic rock in Quruqtagh Xinjiang[J].Journal of Xinjiang University:Natural Science Edition,2013,30(3):354-360.
[33] 张健,张传林,李怀坤,等.再论塔里木北缘阿克苏蓝片岩的时代和成因环境:来自锆石U-Pb年龄、Hf同位素的新证据[J].岩石学报,2014,30(11):3357-3365.
ZHANG Jian,ZHANG Chuanlin,LI Huaikun,et al.Revisit to time and tectonic environment of the Aksu blueschist terrane in northern Tarim,NW China:new evidence from zircon U-Pb age and Hf isotope[J].Acta Petrologica Sinica,2014,30(11):3357-3365.
[34] HE Zhenyu,ZHANG Zeming,ZONG Keqing,et al.Neoproterozoic granulites from the northeastern margin of the Tarim Craton:petrology,zircon U-Pb ages and implications for the Rodinia assembly[J].Precambrian Research,2012,212/213:21-33.
[35] 邬光辉,张承泽,汪海,等.塔里木盆地中部塔参1井花岗闪长岩的锆石SHRIMP U-Pb年龄[J].地 质通报,2009,28(5):568-571.
WU Guanghui,ZHANG Chengze,WANG Hai,et al.Zircon SHRIMP U-Pb age of granodiorite of the Tacan 1 well in the central Tarim Basin,China[J].Geological Bulletin of China,2009,28(5):568-571.
[36] WANG Xuance,LI Xianhua,LI Zhengxiang,et al.Ca.825 Ma komatiitic basalts in South China:first evidence for >1500 ℃ mantle melts by a Rodinian mantle plume [J].Geology,2007,35(12):1103-1106.
[37] WANG Xuance,LI Zhengxiang,LI Xianhua,et al.Geochemical and Hf-Nd isotope data of Nanhua rift sedimentary and volcaniclastic rocks indicate a Neoproterozoic continental flood basalt provenance[J].Lithos,2011,127(3/4):427-440.
[38] 崔海峰,田雷,张年春,等.塔西南坳陷南华纪—震旦纪裂谷分布及其与下寒武统烃源岩的关系[J].石油 学报,2016,37(4):430-438.
CUI Haifeng,TIAN Lei,ZHANG Nianchun,et al.Nanhua-Sinian rift distribution and its relationship with the development of Lower Cambrian source rocks in the southwest depression of Tarim Basin[J].Acta Petrolei Sinica,2016,37(4):430-438.
[39] 石开波,刘波,田景春,等.塔里木盆地震旦纪沉积特征及岩相古地理[J].石油学报,2016,37(11):1343-1360.
SHI Kaibo,LIU Bo,TIAN Jingchun,et al.Sedimentary characteristics and lithofacies paleogeography of Sinian in Tarim Basin[J].Acta Petrolei Sinica,2016,37(11):1343-1360.
[40] 史仁灯,杨经绥,吴才来,等.北祁连玉石沟蛇绿岩形成于晚震旦世的SHRIMP年龄证据[J].地质学报,2004,78(5):649-657.
SHI Rendeng,YANG Jingsui,WU Cailai,et al.Late Sinian Yushigou ophiolite in the North Qilian Mountains:evidences from SHRIMP dating[J].Acta Geologica Sinica,2004,78(5):649-657.
[41] 杨海波,高鹏,李兵,等.新疆西天山达鲁巴依蛇绿岩地质特征[J].新疆地质,2005,23(2):123-126.
YANG Haibo,GAO Peng,LI Bing,et al.The geological character of the Sinian Dalubayi ophiolite in the west Tianshan,Xinjiang[J].Xinjiang Geology,2005,23(2):123-126.
[42] XIAO W J,WINDLEY B F,LIU D Y,et al.Accretionary tectonics of the Western Kunlun Orogen,China:a Paleozoic-Early Mesozoic,long-lived active continental margin with implications for the growth of southern Eurasia[J].The Journal of Geology,2005,113(6):687-705.
[43] 张元元,郭召杰.甘新交界红柳河蛇绿岩形成和侵位年龄的准确限定及大地构造意义[J].岩石学报,2008,24(4):803-809.
ZHANG Yuanyuan,GUO Zhaojie.Accurate constraint on formation and emplacement age of Hongliuhe ophiolite,boundary region between Xinjiang and Gansu Provinces and its tectonic implications[J].Acta Petrologica Sinica,2008,24(4):803-809.
[44] REN Jianye,TAMAKI K,LI Sitian,et al.Late Mesozoic and Cenozoic rifting and its dynamic setting in Eastern China and adjacent areas[J].Tectonophysics,2002,344(3/4):175-205.
[45] 胡见义,牛嘉玉.渤海湾盆地油气聚集理论和勘探实践的再深化——为渤海湾含油气盆地发现40周年而 作[J].石油学报,2001,22(1):1-5.
HU Jianyi,NIU Jiayu.The further deepening of oil-gas accumulation theory and exploratory practice of Bohai Bay Basin[J].Acta Petrolei Sinica,2001,22(1):1-5.
[46] 李德生.松辽盆地的油气形成和分布特征[J].大庆石油地质与开发,1983,2(2):81-89.
LI Desheng.The geological characteristics of hydrocarbon generation and distribution in the Songliao Basin[J].Petroleum Geology & Oilfield Development in Daqing,1983,2(2):81-89.
[47] 夏庆龙,徐长贵.渤海海域复杂断裂带地质认识创新与油气重大发现[J].石油学报,2016,37(增刊1):22-33.
XIA Qinglong,XU Changgui.New geological understandings and major hydrocarbon discoveries in the complex fault zone of Bohai Sea[J].Acta Petrolei Sinica,2016,37(S1):22-33.
[48] 朱光有,陈斐然,陈志勇,等.塔里木盆地寒武系玉尔吐斯组优质烃源岩的发现及其基本特征[J].天然气地球科学,2016,27(1):8-21.
ZHU Guangyou,CHEN Feiran,CHEN Zhiyong,et al.Discovery and basic characteristics of the high-quality source rocks of the Cambrian Yuertusi Formation in Tarim Basin[J].Journal of Natural Gas Geoscience,2016,27(1):8-21.
[49] 何金有,邬光辉,徐备,等.塔里木盆地震旦系-寒武系不整合面特征及油气勘探意义[J].地质科学,2010,45(3):698-706.
HE Jinyou,WU Guanghui,XU Bei,et al.Characteristics and petroleum exploration significance of unconformity between Sinian and Cambrian in Tarim Basin[J].Chinese Journal of Geology,2010,45(3):698-706.
[50] 李朋威,罗平,宋金民,等.微生物碳酸盐岩储层特征与主控因素——以塔里木盆地西北缘上震旦统—下寒武统为例[J].石油学报,2015,36(9):1074-1089.
LI Pengwei,LUO Ping,SONG Jinmin,et al.Characteristics and main controlling factors of microbial carbonate reservoirs:a case study of Upper Sinian-Lower Cambrian in the northwestern margin of Tarim Basin[J].Acta Petrolei Sinica,2015,36(9):1074-1089. |