[1]Zhang Shuichang,Jin Zhijun,Zhang Baomin, et al. The relation between the Cambrian-Ordovician high TOC source rock development and paleoenvironment variations in the Tarim Basin,western China:Carbon and oxygen isotope evidence[J].Acta Geologica Snica,2006,80(3):459-466.[张水昌,金之钧,张宝民,等.塔里木盆地寒武纪—奥陶纪优质烃源岩沉积与古环境变化的关系:碳氧同位素新证据[J].地质学报,2006,80(3):459-466.]
[2]Wu Xiaoqi,Tao Xiaowan,Liu Jingdong.Geochemical characteristics and genetic types of natural gas from Lunnan area in Tarim Basin[J].Natural Gas Geoscience,2014,25(1):53-61.[吴小奇,陶小晚,刘景东.塔里木盆地轮南地区天然气地球化学特征和成因类型[J].天然气地球科学,2014,25(1):53-61.]
[3]Gao Zhiqian,Fan Tailiang,Li Yan, et al. Development pattern and distribution rule of source rock of Cambrian.Ordovician in Tarim Basin[J].Acta Sedimentologica Snica,2006,20(1):69-76.[高志前,樊太亮,李岩,等.塔里木盆地寒武系—奥陶系烃源岩发育模式及分布规律[J].Geoscience,2006,20(1):69-76.]
[4]Zhao Zongju,Zhou Xinyuan,Zheng Xingping, et al. Evidences of chief source rock in Tarim Basin[J].Acta Petrolei Snica,2005,26(3):10-15.[赵宗举,周新源,郑兴平,等.塔里木盆地主力烃源岩的诸多证据[J].石油学报,2005,26(3):10-15.]
[5]Gu Zhidong,Wang Zecheng,Hu Suyun, et al. Tectonic settings of global marine carbonate giant fields and exploration significance[J].Natural Gas Geoscience,2012,23(1):106-117.[谷志东,汪泽成,胡素云,等.全球海相碳酸盐岩巨型油气田发育的构造环境及勘探启示[J].天然气地球科学,2012,23(1):106-117.]
[6]Zhang Yueqiao,Jia Jindou,Jin Yongqiang, et al. Characteristics of Cambrian-Ordovician sedimentary facies in Tadong region and its sedimentary model[J].Natural Gas Geoscience,2007,18(2):229-234.[张月巧,贾进斗,靳久强,等.塔东地区寒武—奥陶系沉积相与沉积演化模式[J].天然气地球科学,2007,18(2):229-234.]
[7]Liu Wei,Zhang Guangya,Pan Wenqing, et al. Lithofacies paleogeography and sedimentary evolution of the Cambrian in Tarim area[J].Journal of paleogeography,2011,13(5):529-538.[刘伟,张光亚,潘文庆,等.塔里木地区寒武纪岩相古地理及沉积演化[J].古地理学报,2011,13(5):529-538.]
[8]Zhao Zongju,Luo Jiahong,Zhang Yunbo, et al. Lithofacies paleogeography of Cambrian sequences in Tarim Basin[J].Acta Petrolei Snica,2011,32(6):937-948.[赵宗举,罗家洪,张运波,等.塔里木盆地寒武纪层序岩相古地理[J].石油学报,2011,32(6):937-948.]
[9]Wu Xingning,Shou Jianfeng,Zhang Huiliang, et al. Characteristics of the petroleum system in Cambrian and Ordovician sequence frameworks of the Tarim Basin and its exploration significance[J].Acta Petrolei Snica,2012,33(2):225-231.[吴兴宁,寿建峰,张惠良,等.塔里木盆地寒武系—奥陶系层序格架中生储盖组合特征与勘探意义[J].石油学报,2012,33(2):225-231.]
[10]Sun Xingli,Chen Jianfa,Liu Wenhui, et al. Geochemical characteristics of cherts of Lower Cambrian in the Tarim Basin and its implication for environmen[J].Petroleum Exploration and Development,2004,31(3):45-48.[孙省利,陈践发,刘文汇,等.塔里木盆地下寒武统硅质岩地球化学特征及其形成环境[J].石油勘探与开发,2004,31(3):45-48.]
[11]Gao Linzhi,Guo Xianpu,Ding Xiaozhong, et al. Nanhuan glaciation event and its stratigraphic correlation in Tarim Plate,China[J].Acta Geoscientica Snica,2013,34(1):39-57.[高林志,郭宪璞,丁孝忠,等.中国塔里木板块南华纪成冰事件及其地层对比[J].地球学报,2013,34(1):39-57.]
[12]Jia Chengzao,Zhang Shiben,Wu Shaozu, et al. Stratigraphy of the Tarim Basin and Adjacent Areas[M].Beijing:Science Press,2004.[贾承造,张师本,吴绍祖,等.塔里木盆地及周边地层[M].北京:科学出版社,2004.]
[13]Zhu W B,Zheng B,Shu L S, et al. Neoproterozoic tectonic evolution of the Precambrian Aksu blueschist terrane,northwestern Tarim,China:Insights from LA-ICP-MS zircon U–Pb ages and geochemical data[J].Precambrian Research,2011,185(3):215-230.
[14]Zhang C L,Li Z X,Li X H, 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.
[15]Yang Ruidong,Zhang Chuanlin,Luo Xinyong, et al. New evidences on Neoproterozoic Hankalchough glaciation in Quruqtagh,Xinjiang,west China[J].Geological review,2007,53(2):228-233.[杨瑞东,张传林,罗新荣,等.新疆库鲁克塔格地区新元古代末期汉格尔乔克冰期成因新证据[J].地质论评,2007,53(2):228-233.]
[16]Wang Fei,Wang Bo,Shu Liangshu, et al. Continental tholeitic basalt of the Akesu area and its implication for the Neoproterozoic rifting in the northern Tarim[J].Acta Petrologica Sinica,2010,26(2):547-558.[王飞,王博,舒良树.塔里木西北缘阿克苏地区大陆拉斑玄武岩对新元古代裂解事件的制约[J].岩石学报,2010,26(2):547-558.]
[17]Li Xiangmin,Xia Lin,Xia Zuchun, et al. Geochemical characteristics and petrogenesis of Neoproterozoic-Early Cambrian volcanic rocks in Tianshan area[J].Acta Petrologica et Mineralogica,2006,25(5):412-422.[李向民,夏林,夏祖春,等.天山地区新元古代—早寒武世火山岩地球化学和岩石成因[J].岩石矿物学杂志,2006,25(5):412-422.]
[18]Li Z X,Powell C M A.An outline of the palaeogeographic evolution of the Australasian region since the beginning of the Neoproterozoic[J].Earth-Science Reviews,2001,53(3):237-277.
[19]Zhou Xiaobei,Li Jianghai,Fu Chenjian, et al. Discussions on the Cryogenian-Cambrian tectonic-sedimentary event and tectonic setting of northern Tarim Basin[J].Geology in China,2012,39(4):900-910.[周肖贝,李江海,傅臣建,等.塔里木西北缘南华纪—寒武纪构造背景及构造—沉积事件探讨[J].中国地质,2012,39(4):900-910.]
[20]Li Yuejun,Sun Longde,Hu Shiling, et al. 40Ar-39Ar geochronology of the granite and diorite revealed at the bottom of Tacan 1,the deepest well in China[J].Acta Petrologica Sinica,2003,19(3):530-536.[李曰俊,孙龙德,胡世玲,等.塔里木盆地塔参1井底部花岗闪长岩的40Ar/39Ar年代学研究.岩石学报,2003,19(3):530-536.]
[21]Tyson R V.The genesis and palynofacies characteristics of marine petroleum source rocks[J].Geological Society,1987,26(1):47-67.
[22]Bouloubassi I,Rullktter J,Meyers P A.Origin and transformation of organic matter in Pliocene-Pleistocene Mediterranean sapropels:Organic geochemical evidence reviewed[J].Marine Geology,1999,153(1):177-197.
[23]Liang Digang,Guo Tonglou,Bian Lizeng, et al. Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,southern China (Part 3):Controlling factors on the sedimentary facies and development of Paleozoic Marine source rocks[J].Marine Origin Petroleum Geology,2009,14(2):1-19.[梁狄刚,郭彤楼,边立曾,等.中国南方海相生烃成藏研究的若干新进展 (三) :南方四套区域性海相烃源岩的沉积相及发育的控制因素[J].海相油气地质,2009,14(2):1-19.]
[24]Zhang Baomin,Zhang Shuichang,Bian Lizeng, et al. Initial discussion on the developmental model of Neoproterozoic-Lower Paleozoic marine source rocks in south China[J].Science Bulletin,2007,52(supplementⅠ):58-69.[张宝民,张水昌,边立曾,等.浅析中国新元古—下古生界海相烃源岩的发育模式[J].科学通报,2007,52(增刊Ⅰ):58-69.]
[25]Yang Yongjian,Liu Jiaduo,Tian Jingchun, et al. Sequence Lithofacies paleogeography of Cambrian in Tarim Basin[J].Natural Gas Geoscience,2011,22(3):450-459.[杨永剑,刘家铎,田景春,等.塔里木盆地寒武纪层序岩相古地理特征[J].天然气地球科学,2011,22(3):450-459.] |