塔里木盆地南华纪古裂谷对寒武系沉积的控制及勘探意义

doi:10.7623/syxb202011001

石油学报 ›› 2020, Vol. 41 ›› Issue (11): 1293-1308.DOI: 10.7623/syxb202011001

• 地质勘探 • 下一篇

塔里木盆地南华纪古裂谷对寒武系沉积的控制及勘探意义

易士威¹, 李明鹏¹, 郭绪杰², 范土芝², 杨帆², 方辉², 缪卫东¹, 林世国¹, 高阳¹, 李德江¹

1. 中国石油勘探开发研究院北京 100083;
2. 中国石油勘探与生产分公司北京 100007

收稿日期:2020-04-15 修回日期:2020-08-20 出版日期:2020-11-25 发布日期:2020-12-11
通讯作者: 李明鹏,男,1989年2月生,2012年获中国地质大学(武汉)学士学位,2015年获中国石油大学(华东)硕士学位,现为中国石油勘探开发研究院工程师,主要从事油气地质综合研究及勘探部署工作。Email:limingpeng@petrochina.com.cn
作者简介:易士威,男,1964年1月生,1986年获中国地质大学(武汉)学士学位,2006年获成都理工大学博士学位,现为中国石油勘探开发研究院教授级高级工程师,主要从事油气地质综合研究及勘探部署工作。Email:ktb_ysw@petrochina.com.cn
基金资助:
国家科技重大专项（2016ZX05007-002，2016ZX05007-003）资助。

Control of the Nanhua paleo-rift on Cambrian sedimentation and its exploration significance in Tarim Basin

Yi Shiwei¹, Li Mingpeng¹, Guo Xujie², Fan Tuzhi², Yang Fan², Fang Hui², Miao Weidong¹, Lin Shiguo¹, Gao Yang¹, Li Dejiang¹

1. PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China;
2. PetroChina Exploration&Production Company, Beijing 100083, China

Received:2020-04-15 Revised:2020-08-20 Online:2020-11-25 Published:2020-12-11

摘要/Abstract

摘要：

塔里木盆地前寒武系经历了南华纪断陷构造沉降和震旦纪坳陷热沉降2个阶段，发育众多不同走向、不同规模的古裂谷。根据古裂谷的走向、规模、性质及其对上覆沉积的控制作用可将其分为台间古裂谷和台内古裂谷2种类型。众多古裂谷形成的垒-堑相间的古构造对寒武纪岩相古地理具有明显的控制作用，即古裂谷控制了寒武系的生烃中心、优质储层和优质盖层的发育。在古裂谷之上继承性发育的古地貌低洼区是寒武系玉尔吐斯组优质烃源灶的发育区。在裂谷肩部形成的古地貌高隆区则往往沉积丘滩建造，为优质储层发育区。满加尔台间古裂谷的两侧肩部由于长期处于稳定发育的古地貌高部位，可形成沿该古地貌高呈SN向展布的镶边台地边缘丘滩建造，由此导致塔西地区、罗西地区在寒武纪吾松格尔组—阿瓦塔格组沉积期形成封闭的台地环境，并在轮台—古城一线以西沉积大面积的膏盐岩优质盖层。在台内古裂谷之上，玉尔吐斯组烃源岩相对较厚，成为有利生烃中心；在古裂谷间的相对古地貌高部位，肖尔布拉克组白云岩滩相储层更加发育。二者与上覆的中寒武统膏盐岩盖层构成优越的生-储-盖组合，是寒武系盐下油气最有利的成藏区，也是形成大气藏和实现勘探突破最有利的地区。

关键词: 塔里木盆地, 古裂谷, 沉积响应, 生烃中心, 边缘丘滩, 成藏模式

Abstract:

Tarim Basin has experienced two stages of the tectonic subsidence in the Precambrian, i.e., the Nanhua fault depression and the thermal subsidence of the Sinian depression, and also developed many paleo-rifts with different strikes and scales. According to the strike, scale, property and control of overlying sediments, the paleo-rift can be divided into two types:inter-platform rift and intra-platform rift. The horst-graben paleo-structure formed by many paleo-rifts has obvious control on the Cambrian lithofacies and palaeogeography, i.e., the paleo-rifts control the development of the Cambrian hydrocarbon generation centers, high-quality reservoirs and caps. The high-quality hydrocarbon kitchen of Cambrian Yuertusi Formation is developed in the low-lying parts of paleo-landforms inherited and developed above the paleo-rifts. Reefs and shoals are often deposited in the paleo-uplift areas at the shoulders of the rift, where high-quality reservoirs are developed. Since the shoulders on both sides of the inter-platform rift in Manjiaer are located in the high part of the paleo-landform developed steadily for a long time, they can form the rimmed marginal reefs and shoals distributed in a south-north direction along the high part of the paleo-landform, resulting in a closed platform environment formed during the deposition period of the Cambrian Wusonggeer-Awatage formations in Taxi and Luoxi areas and a large area of high-quality gypsum caprock deposited in the west of Luntai-Gucheng. Above the intra-platform, the source rocks of Yuertusi Formation are relatively thick and become a favorable hydrocarbon generation center. In addition, the dolomite shoal facies reservoirs of Xiaoerbulake Formation are more developed in the relatively high parts between the paleo-rifts. The superior combination of the two and the upper Middle Cambrian gypsum salt caprock is the most favorable area for Cambrian presalt hydrocarbon accumulation, and also the most favorable area for forming giant gas reservoir and achieving exploration breakthrough.

Key words: Tarim Basin, paleo-rift, sedimentary response, hydrocarbon generation center, marginal reef and shoal, accumulation model

中图分类号:

TE121.2

易士威, 李明鹏, 郭绪杰, 范土芝, 杨帆, 方辉, 缪卫东, 林世国, 高阳, 李德江. 塔里木盆地南华纪古裂谷对寒武系沉积的控制及勘探意义[J]. 石油学报, 2020, 41(11): 1293-1308.

Yi Shiwei, Li Mingpeng, Guo Xujie, Fan Tuzhi, Yang Fan, Fang Hui, Miao Weidong, Lin Shiguo, Gao Yang, Li Dejiang. Control of the Nanhua paleo-rift on Cambrian sedimentation and its exploration significance in Tarim Basin[J]. Acta Petrolei Sinica, 2020, 41(11): 1293-1308.

参考文献

[1] 贾承造. 中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997.
JIA Chengzao.Tectonic characteristics and petroleum,Tarim Basin,China[M].Beijing:Petroleum Industry Press,1997.
[2] 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.
[3] 庞雄奇,陈君青,李素梅,等.塔里木盆地特大型海相油田原油来源——来自深部低TOC烃源岩的证据与相对贡献评价[J].石油学报,2018,39(1):23-41,91.
PANG Xiongqi,CHEN Junqing,LI Sumei,et al.Crude oil sources of giant marine oilfield in Tarim Basin:evidences and relative contribution evaluation of deep present-day low-TOC source rocks[J].Acta Petrolei Sinica,2018,39(1):23-41,91.
[4] 王招明,谢会文,陈永权,等.塔里木盆地中深1井寒武系盐下白云岩原生油气藏的发现与勘探意义[J].中国石油勘探,2014,19(2):1-13.
WANG Zhaoming,XIE Huiwen,CHEN Yongquan,et al.Discovery and exploration of cambrian subsalt dolomite original hydrocarbon reservoir at Zhongshen-1 Well in Tarim Basin[J].China Petroleum Exploration,2014,19(2):1-13.
[5] 易士威,李明鹏,郭绪杰,等.塔里木盆地寒武系盐下勘探领域的重大突破方向[J].石油学报,2019,40(11):1281-1295.
YI Shiwei,LI Mingpeng,GUO Xujie,et al.Breakthrough direction of Cambrian pre-salt exploration fields in Tarim Basin[J].Acta Petrolei Sinica,2019,40(11):1281-1295.
[6] 石开波,刘波,刘红光,等.塔里木盆地东北缘库鲁克塔格地区新元古代构造-沉积演化[J].地学前缘,2017,24(1):297-307.
SHI Kaibo,LIU Bo,LIU Hongguang,et al.Neoproterozoic tectono-sedimentary evolution in Quruqtagh area,NE Tarim Basin,Xinjiang,China[J].Earth Science Frontiers,2017,24(1):297-307.
[7] 吴林,管树巍,杨海军,等.塔里木北部新元古代裂谷盆地古地理格局与油气勘探潜力[J].石油学报,2017,38(4):375-385.
WU Lin,GUAN Shuwei,YANG Haijun,et al.The paleogeographic framework and hydrocarbon exploration potential of Neoproterozoic rift basin in northern Tarim Basin[J].Acta Petrolei Sinica,2017,38(4):375-385.
[8] 任荣,管树巍,吴林,等.塔里木新元古代裂谷盆地南北分异及油气勘探启示[J].石油学报,2017,38(3):255-266.
REN Rong,GUAN Shuwei,WU Lin,et al.The north-south differentiation characteristic and its enlightenment on oil-gas exploration of the Neoproterozoic rift basin,Tarim Basin[J].Acta Petrolei Sinica,2017,38(3):255-266.
[9] 李勇,陈才,冯晓军,等.塔里木盆地西南部南华纪裂谷体系的发现及意义[J].岩石学报,2016,32(3):825-832.
LI Yong,CHEN Cai,FENG Xiaojun,et al.New discovery of Nanhuaian rift system in southwestern Tarim basin and its geological significance[J].Acta Petrologica Sinica,2016,32(3):825-832.
[10] 周肖贝,李江海,王洪浩,等.塔里木盆地南华纪-震旦纪盆地类型及早期成盆构造背景[J].地学前缘,2015,22(3):290-298.
ZHOU Xiaobei,LI Jianghai,WANG Honghao,et al.The type of prototypic basin and tectonic setting of Tarim Basin formation from Nanhua to Sinian[J].Earth Science Frontiers,2015,22(3):290-298.
[11] 石开波,刘波,姜伟民,等.塔里木盆地南华纪-震旦纪构造-沉积格局[J].石油与天然气地质,2018,39(5):862-877.
SHI Kaibo,LIU Bo,JIANG Weimin,et al.Nanhua-Sinian tectono-sedimentary framework of Tarim Basin,NW China[J].Oil & Gas Geology,2018,39(5):862-877.
[12] 周肖贝,李江海,傅臣建,等.塔里木盆地北缘南华纪-寒武纪构造背景及构造-沉积事件探讨[J].中国地质,2012,39(4):900-911.
ZHOU Xiaobei,LI Jianghai,FU Chenjian,et al.A discussions on the Cryogenian-Cambrian tectonic-sedimentary event and tectonic setting of northern Tarim Basin[J].Geology in China,2012,39(4):900-911.
[13] 王杰琼,刘波,罗平,等.塔里木盆地西北缘震旦系混积岩类型及成因[J].成都理工大学学报:自然科学版,2014,41(3):339-346.
WANG Jieqiong,LIU Bo,LUO Ping,et al.Classification and genesis of Sinian mixosedimentite from northwest margin of Tarim Basin,China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2014,41(3):339-346.
[14] 童勤龙,卫魏,徐备.塔里木板块西南缘新元古代沉积相和冰期划分[J].中国科学:地球科学,2013,43(5):703-715.
TONG Qinlong,WEI Wei,XU Bei.Neoproterozoic sedimentary facies and glacial periods in the southwest of Tarim block[J].Science China:Earth Sciences,2013,56(6):901-912.
[15] 魏震,郭瑞清,赵新生,等.库鲁克塔格地区南华系贝义西组沉积环境及对南华纪裂谷盆地演化的指示[J].新疆地质,2016,34(3):331-337.
WEI Zhen,GUO Ruiqing,ZHAO Xinsheng,et al.Sedimentary environment of Nanhuaan Bayisi Formation in Quruqtagh domain and its implications on the evolution of the Nanhua rift basin[J].Xinjiang Geology,2016,34(3):331-337.
[16] 尹崇玉,高林志.中国南华系的范畴、时限及地层划分[J].地层学杂志,2013,37(4):534-541.
YIN Chongyu,GAO Linzhi.Definition,time limit and stratigraphic subdivision of the Nanhuan system in China[J].Journal of Stratigraphy,2013,37(4):534-541.
[17] 康建威,牟传龙,周恳恳,等.塔里木盆地北缘阿克苏地区震旦系露头层序地层研究[J].沉积与特提斯地质,2016,36(2):47-54.
KANG Jianwei,MOU Chuanlong,ZHOU Kenken,et al.Sequence stratigraphic analysis of the Sinian strata in the Aksu region,Xinjiang[J].Sedimentary Geology and Tethyan Geology,2016,36(2):47-54.
[18] 何景文,朱文斌,郑碧海,等.塔里木西北缘阿克苏地区震旦系苏盖特布拉克组沉积物源分析:碎屑锆石年代学证据[J].地质学报,2015,89(1):149-162.
HE Jingwen,ZHU Wenbin,ZHENG Bihai,et al.Provenance of sinian sugetbrak sedimentary rocks in the Aksu area,NW tarim:evidence from detrital zircon geochronology[J].Acta Geologica Sinica,2015,89(1):149-162.
[19] 张传林,叶海敏,王爱国,等.塔里木西南缘新元古代辉绿岩及玄武岩的地球化学特征:新元古代超大陆(Rodinia)裂解的证据[J].岩石学报,2004,20(3):473-482.
ZHANG Chuanlin,YE Haimin,WANG Aiguo,et al.Geochemistry of the Neoproterozoic diabase and basalt in south of Tarim plate:evidence for the Neoproterozoic breakup of the Rodinia super-continent in south of Tarim[J].Acta Petrologica Sinica,2004,20(3):473-482.
[20] 姜海健,陈强路,杨鑫,等.塔里木盆地新元古代裂谷盆地层序样式[J].地质学报,2017,91(3):588-604.
JIANG Haijian,CHEN Qianglu,YANG Xin,et al.The style of sequence stratigraphy of neoproterozoic rift basin in the Tarim Basin[J].Acta Geologica Sinica,2017,91(3):588-604.
[21] 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.
[22] 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.
[23] 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.
[24] 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.
GAO Linzhi,GUO Xianpu,DING Xiaozhong,et al.Nanhuan glaciation event and its stratigraphic correlation in Tarim plate,China[J].Acta Geoscientia Sinica,2013,34(1):39-57.
[25] TURNER S A.Sedimentary record of Late Neoproterozoic rifting in the NW Tarim Basin,China[J].Precambrian Research,2010,181(1/4):85-96.
[26] WANG Chao,LIU Liang,WANG Yonghe,et al.Recognition and tectonic implications of an extensive Neoproterozoic volcano-sedimentary rift basin along the southwestern margin of the Tarim craton,northwestern China[J].Precambrian Research,2015,257:65-82.
[27] WANG Chao,ZHANG Jiheng,LI Meng,et al.Generation of ca.900-870 Ma bimodal rifting volcanism along the southwestern margin of the Tarim craton and its implications for the Tarim-North China connection in the Early Neoproterozoic[J].Journal of Asian Earth Sciences,2015,113:610-625.
[28] 石书缘,刘伟,黄擎宇,等.塔里木盆地北部震旦系齐格布拉克组白云岩储层特征及成因[J].天然气地球科学,2017,28(8):1226-1234.
SHI Shuyuan,LIU Wei,HUANG Qingyu,et al.Dolostone reservoir characteristic and its formation mechanismin Qigebulake Formtion,Sinian,North Tarim Basin[J].Natural Gas Geoscience,2017,28(8):1226-1234.
[29] 赵明胜,田景春,苏炳睿,等.塔东北库鲁克塔格地区震旦-奥陶纪地质事件及生储盖组合[J].中国地质,2018,45(3):591-603.
ZHAO Mingsheng,TIAN Jingchun,SU Bingrui,et al.The geological event and the assemblage of source-reservoir-seal rock during the Sinian-Ordovician period in Kuruktag region of northeastern Tarim Basin[J].Geology in China,2018,45(3):591-603.
[30] 韩强,杨子川,李宗杰,等.塔里木盆地沙雅隆起北部震旦纪地层特征与锆石U-Pb年龄约束[J].地层学杂志,2017,41(4):428-436.
HAN Qiang,YANG Zichuan,LI Zongjie,et al.Sinian stratigraphy and zircon U-Pb ages from the Shaya uplift of the Tarim Basin,NW China[J].Journal of Stratigraphy,2017,41(4):428-436.
[31] 杨鑫,李慧莉,张仲培,等.塔里木新元古代盆地演化与下寒武统烃源岩发育的构造背景[J].地质学报,2017,91(8):1706-1719.
YANG Xin,LI Huili,ZHANG Zhongpei,et al.Evolution of Neoproterozoic Tarim Basin in northwestern China and tectonic background of the Lower Cambrian hydrocarbon source rocks[J].Acta Geologica Sinica,2017,91(8):1706-1719.
[32] 韩剑发,苏洲,陈利新,等.塔里木盆地台盆区走滑断裂控储控藏作用及勘探潜力[J].石油学报,2019,40(11):1296-1310.
HAN Jianfa,SU Zhou,CHEN Lixin,et al.Reservoir-controlling and accumulation-controlling of strike-slip faults and exploration potential in the platform of Tarim Basin[J].Acta Petrolei Sinica,2019,40(11):1296-1310.
[33] 马永生,何治亮,赵培荣,等.深层-超深层碳酸盐岩储层形成机理新进展[J].石油学报,2019,40(12):1415-1425.
MA Yongsheng,HE Zhiliang,ZHAO Peirong,et al.A new progress in formation mechanism of deep and ultra-deep carbonate reservoir[J].Acta Petrolei Sinica,2019,40(12):1415-1425.
[34] 何金有,李洪辉,罗平,等.塔东低凸起震旦系断陷台地沉积特征及发育模式[J].地质与勘探,2017,53(2):361-370.
HE Jinyou,LI Honghui,LUO Ping,et al.Sedimentary characteristics and evolution models of the Sinian rift platform in the low-uplift,eastern Tarim Basin[J].Geology and Exploration,2017,53(2):361-370.
[35] 冯许魁,刘永彬,韩长伟,等.塔里木盆地震旦系裂谷发育特征及其对油气勘探的指导意义[J].石油地质与工程,2015,29(2):5-10.
FENG Xukui,LIU Yongbin,HAN Changwei,et al.Sinian rift valley development characteristics in Tarim Basin and its guidance on hydrocarbon exploration[J].Petroleum Geology and Engineering,2015,29(2):5-10.
[36] 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.
[37] 杨鑫,李慧莉,岳勇,等.塔里木盆地震旦纪末地层-地貌格架与寒武纪初期烃源岩发育模式[J].天然气地球科学,2017,28(2):189-198.
YANG Xin,LI Huili,YUE Yong,et al.The strata and palaeo-geomorphology framework at the end of Neoproterozoic and development mode of source rocks at the beginning of Cambrian[J].Natural Gas Geoscience,2017,28(2):189-198.

塔里木盆地南华纪古裂谷对寒武系沉积的控制及勘探意义

Control of the Nanhua paleo-rift on Cambrian sedimentation and its exploration significance in Tarim Basin

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