南海边缘海构造旋回对沉积充填的控制——以礼乐盆地新生代沉积为例

doi:10.7623/syxb201604006

石油学报 ›› 2016, Vol. 37 ›› Issue (4): 474-482.DOI: 10.7623/syxb201604006

南海边缘海构造旋回对沉积充填的控制——以礼乐盆地新生代沉积为例

王一博, 张功成, 赵志刚, 谢晓军, 刘世翔, 管红, 董伟, 宋双

中海油研究总院北京 100028

收稿日期:2015-09-30 修回日期:2016-03-12 出版日期:2016-04-25 发布日期:2016-05-06
通讯作者: 王一博,女,1978年11月生,2001年获大庆石油学院学士学位,2008年获中国石油大学(北京)博士学位,现为中海油研究总院地质工程师,主要从事石油地质研究工作。Email:wangyb5@cnooc.com.cn
作者简介:王一博,女,1978年11月生,2001年获大庆石油学院学士学位,2008年获中国石油大学(北京)博士学位,现为中海油研究总院地质工程师,主要从事石油地质研究工作。Email:wangyb5@cnooc.com.cn
基金资助:
国家重大科技专项(2008ZX05025,2011ZX05025)、国家自然科学基金重大研究计划项目(No.91528303)和中海石油(中国)有限公司科技项目"南海新生代盆地构造沉积演化及资源潜力分析"资助。

The control for tectonic cycle of marginal sea on sedimentary fill in South China Sea:a case study of Cenozoic sediment in Lile Basin

Wang Yibo, Zhang Gongcheng, Zhao Zhigang, Xie Xiaojun, Liu Shixiang, Guan Hong, Dong Wei, Song Shuang

CNOOC Research Institute, Beijing 100028, China

Received:2015-09-30 Revised:2016-03-12 Online:2016-04-25 Published:2016-05-06

摘要/Abstract

摘要：

礼乐盆地是在南海边缘海构造旋回控制下形成的沉积盆地,受古南海消亡与新南海扩张影响,盆地自晚白垩世以来经历了晚白垩世-早渐新世漂移前、晚渐新世-中中新世漂移和晚中新世-现今漂移后共3期区域演化阶段。古新世-早渐新世,礼乐盆地以滨浅海沉积为主,主要发育三角洲-扇三角洲-水下扇-盆底扇-滨海-浅海沉积体系;晚渐新世-中中新世,沉积物源供给缺乏,以滨浅海和半深海沉积为主,盆地北部发育大型碳酸盐台地;晚中新世以来,沉积物源主要来自盆地东南侧及内部火山,发育水下扇-浅海-半深海-碳酸盐台地沉积体系,以浅海和半深海沉积为主。礼乐盆地具有相对较好的烃源岩、有利的储集相带和良好的区域盖层,油气资源勘探潜力较大。

关键词: 边缘海构造旋回, 礼乐盆地, 新生代, 区域演化, 沉积充填

Abstract:

Lile Basin is a sedimentary basin formed under the control of the tectonic cycle of marginal sea in South China Sea. Influenced by the disappearance of Paleo-South China Sea and the expansion of New South China Sea, Lile Basin has undergone three regional evolution since the Late Cretaceous, i.e., the stage prior to Late Cretaceous-Early Oligocene drifting, the Late Oligocene-Middle Miocene drifting stage, and the stage posterior to Late Miocene-current drifting stage. In the Paleocene-Early Oligocene, Lile Basin was dominated by littoral-neritic sediments, where the delta-fan delta-submarine fan-basin floor fan-littoral-neritic sedimentary system was mainly developed. In the Late Oligocene-Middle Miocene, due to lack of sediment provenance, Lile Basin was dominated by littoral-neritic and bathyal sediments, where a large-scale carbonate platform was developed in the northern basin. Since the Late Miocene, sedimentary provenances were mainly sourced from the southeastern basin and internal volcanoes, where the submarine fan-neritic-bathyal-carbonate platform sedimentary system was developed and mainly made up of neritic-bathyal sediments. Lile Basin has relatively good source rocks, favorable reservoir facies belts and regional caps, indicating a huge hydrocarbon resource potential.

Key words: tectonic cycle of marginal sea, Lile Basin, Cenozoic, regional evolution, sedimentary filling

中图分类号:

TE122

王一博, 张功成, 赵志刚, 谢晓军, 刘世翔, 管红, 董伟, 宋双. 南海边缘海构造旋回对沉积充填的控制——以礼乐盆地新生代沉积为例[J]. 石油学报, 2016, 37(4): 474-482.

Wang Yibo, Zhang Gongcheng, Zhao Zhigang, Xie Xiaojun, Liu Shixiang, Guan Hong, Dong Wei, Song Shuang. The control for tectonic cycle of marginal sea on sedimentary fill in South China Sea:a case study of Cenozoic sediment in Lile Basin[J]. Acta Petrolei Sinica, 2016, 37(4): 474-482.

参考文献

[1] 张功成,王璞珺,吴景富,等.边缘海构造旋回:南海演化的新模式[J].地学前缘,2015,22(3):27-37.
Zhang Gongcheng,Wang Pujun,Wu Jingfu,et al.Tectonic cycle of marginal oceanic basin:a new evolution model of the South China Sea[J].Earth Science Frontiers,2015,22(3):27-37.
[2] 张伟,何家雄,颜文,等.中国边缘海盆地构造演化与油气分布富集规律[J].西南石油大学学报:自然科学版,2014,36(2):9-23.
Zhang Wei,He Jiaxiong,Yan Wen,et al.Characteristics of tectonic evolution and distribution and enrichment patterns of oil and gas in the Chinese marginal basin[J]. Journal of Southwest Petroleum University:Science & Technology Edition,2014,36(2):9-23.
[3] 张功成,屈红军,刘世翔,等.边缘海构造旋回控制南海深水区油气成藏[J].石油学报,2015,36(5):533-545.
Zhang Gongcheng,Qu Hongjun,Liu Shixiang,et al.Tectonic cycle of marginal sea controlled the hydrocarbon accumulation in deep-water areas of South China Sea[J].Acta Petrolei Sinica,2015,36(5):533-545.
[4] 姚永坚,姜玉坤,曾祥辉.南沙海域新生代构造运动特征[J].中国海上油气(地质),2002,16(2):113-117.
Yao Yongjian,Jiang Yukun,Zeng Xianghui.Cenozoic tectonic movements in Nansha area,South China Sea[J].China Offshore Oil and Gas (Geology),2002,16(2):113-117.
[5] Taylor B,Hayes D E.Origin and history of the South China Sea Basin[M]//Hayes D E.The tectonic and geologic evolution of Southeast Asian Seas and Islands:Part 2.Washington,DC:American Geophysical Union,1983.
[6] Tamaki K,Honza E.Global tectonics and formation of marginal basins:role of the western Pacific[J].Episodes,1991,14(3):224-230.
[7] Ben-Avraham Z,Uyeda S.The evolution of the China basin and the Mesozoic paleogeography of Borneo[J].Earth and Planetary Science Letters,1973,18(2):365-376.
[8] 姚伯初.南海海盆新生代的构造演化史[J].海洋地质与第四纪地质,1996,16(2):1-13.
Yao Bochu.Tectonic evolution of the South China Sea in Cenozoic[J].Marine Geology & Quaternary Geology,1996,16(2):1-13.
[9] 谢锦龙,黄冲,向峰云.南海西部海域新生代构造古地理演化及其对油气勘探的意义[J].地质科学,2008,43(1):133-153.
Xie Jinlong,Huang Chong,Xiang Fengyun.Evolution of Cenozoic tectono-palaeogeography and its petroleum significance in the western South China Sea[J].Chinese Journal of Geology,2008,43(1):133-153.
[10] 姚伯初,万玲,刘振湖.南海海域新生代沉积盆地构造演化的动力学特征及其油气资源[J].地球科学——中国地质大学学报,2004,29(5):543-549.
Yao Bochu,Wan Ling,Liu Zhenhu.Tectonic dynamics of Cenozoic sedimentary basins and hydrocarbon resources in the South China Sea[J].Earth Science:Journal of China University of Geosciences,2004,29(5):543-549.
[11] 龚铭,李唐根,伍泓.南沙海域构造演化与油气资源前景[J].天然气工业,2004,24(3):32-35.
Gong Ming,Li Tanggen,Wu Hong.Tectonic evolution and hydrocarbon potential of Nansha offshore area[J].Natural Gas Industry,2004,24(3):32-35.
[12] 高红芳,曾祥辉,刘振湖,等.南海礼乐盆地沉降史模拟及构造演化特征分析[J].大地构造与成矿学,2005,29(3):385-390.
Gao Hongfang,Zeng Xianghui,Liu Zhenhu,et al.Simulating of subsidence history and analysis of tectonic evolutionary characteristics of Liyue Basin in South China Sea[J].Geotectonica et Metallogenia,2005,29(3):385-390.
[13] 孙龙涛,孙珍,周蒂,等.南沙海区礼乐盆地沉积地层与构造特征分析[J].大地构造与成矿学,2008,32(2):151-158.
Sun Longtao,Sun Zhen,Zhou Di,et al.Stratigraphic and structural characteristics of Lile Basin in Nansha area[J].Gentectonica et Metallogenia,2008,32(2):151-158.
[14] 李鹏春,赵中贤,张翠梅,等.南沙海域礼乐盆地沉积过程和演化[J].地球科学——中国地质大学学报,2011,36(5):837-844.
Li Pengchun,Zhao Zhongxian,Zhang Cuimei,et al.Depositional process and evolution of Liyue Basin in Southern South China Sea[J].Earth Science:Journal of China University of Geosciences,2011,36(5):837-844.
[15] 谢晓军,张功成,刘世翔,等.礼乐盆地漂移前的位置探讨[J].科学技术与工程,2015,15(2):8-13.
Xie Xiaojun,Zhang Gongcheng,Liu Shixiang,et al.Discussion the pre-drifting position of the Liyue Basin[J].Science Technology and Engineering,2015,15(2):8-13.
[16] Tayler B,Hayes D E.The tectonic evolution of the South China Basin[M]//Hayes D E.The tectonic and geologic evolution of Southeast Asian Seas and Islands:Part 2.Washington,DC:American Geophysical Union,1983.
[17] Holloway N H.North Palawan block,Philippines:its relation to Asian mainland and role in evolution of South China Sea[J].AAPG Bulletin,1982,66(9):1335-1383.
[18] Briais A,Patriat P,Tapponnier P.Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea:implications for the Tertiary tectonics of Southeast Asia[J].Journal of Geophysical Research,1993,98(B4):6299-6328.
[19] Zhou Di,Ru Ke,Chen Hanzong.Kinematics of Cenozoic extension on the South China Sea continental margin and its implications for the tectonic evolution of the region[J].Tectonophysics,1995,251(1/4):161-177.
[20] Schlüter H U,Hinz K,Block M.Tectono-stratigraphic terranes and detachment faulting of the South China Sea and Sulu Sea[J].Marine Geology,1996,130(1/2):39-51,58-78.
[21] Kudrass H R,Wiedicke M,Cepeck P,et al.Mesozoic and Cainozoic rocks dredged from the South China Sea (Reed bank Area) and Sulu Sea and their significance for plate-tectonic reconstructions[J].Marine and Petroleum Geology,1986,3(1):19-30.
[22] 张莉,李文成,李国英,等.南沙东北部海域礼乐盆地含油气组合静态地质要素分析[J].中国地质,2004,31(3):320-324.
Zhang Li,Li Wencheng,Li Guoying,et al.Analysis of static geological elements of petroleum-bearing combinations in the Lile Basin,northeastern Nansha[J].Geology in China,2004,31(3):320-324.
[23] 张莉,李文成,曾祥辉.礼乐盆地地层发育特征及其与油气的关系[J].石油实验地质,2003,25(5):469-472.
Zhang Li,Li Wencheng,Zeng Xianghui.Stratigraphic sequence and hydrocarbon potential in Lile Basin[J].Petroleum Geology & Experiment,2003,25(5):469-472.
[24] 张莉,沙志彬,王立飞.南沙海域礼乐盆地中生界油气资源潜力[J].海洋地质与第四纪地质,2007,27(4):97-102.
Zhang Li,Sha Zhibin,Wang Lifei.Hydrocarbon resources potential of Mesozoic in Liyue Basin,northeastern Nansha Sea areas[J].Marine Geology & Quaternary Geology, 2007,27(4):97-102.
[25] 孙龙涛,孙珍,詹文欢,等.南沙海域礼乐盆地油气资源潜力[J].地球科学——中国地质大学学报,2010,35(1):137-145.
Sun Longtao,Sun Zhen,Zhan Wenhuan,et al.Petroleum potential prediction of the Lile Basin in Nansha[J].Earth Science:Journal of China University of Geosciences,2010,35(1):137-145.
[26] 孙晓猛,张旭庆,张功成,等.南海北部新生代盆地基底结构及构造属性[J].中国科学:地球科学,2014,44(6):1312-1323.
Sun Xiaomeng,Zhang Xuqing,Zhang Gongcheng,et al.Texture and tectonic attribute of Cenozoic basin basement in the northern South China Sea[J].Science China:Earth Sciences,2014,57(6):1199-1211.
[27] 蔡周荣,张毅,刘维亮,等.南海的形成演化与新特提斯在南海的重新活化[J].沉积与特提斯地质,2008,28(3):21-24.
Cai Zhourong,Zhang Yi,Liu Weiliang,et al.Relationship between the formation and evolution of the South China Sea and reactivation of the Neo-Tethys[J].Sedimentary Geology and Tethyan Geology,2008,28(3):21-24.

南海边缘海构造旋回对沉积充填的控制——以礼乐盆地新生代沉积为例

The control for tectonic cycle of marginal sea on sedimentary fill in South China Sea:a case study of Cenozoic sediment in Lile Basin

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	张功成. 南海渐进式边缘海构造旋回控制深水油气成藏理论[J]. 石油学报, 2023, 44(4): 569-582.
[2]	朱明, 袁波, 梁则亮, 杨迪生, 唐雪颖. 准噶尔盆地周缘断裂属性与演化[J]. 石油学报, 2021, 42(9): 1163-1173.
[3]	康琳, 吕丁友, 尚锁贵, 高京华, 张江涛. 辽东湾坳陷新生代构造变形特征及营潍断裂带的表现[J]. 石油学报, 2019, 40(S2): 79-90.
[4]	陈林, 陆永潮, 林卫兵, 邢凤存, 陈平, 刘璐, 胡海燕, 魏巍. 鄂尔多斯盆地西南部延长组长8油层组层序地层特征及沉积充填模式[J]. 石油学报, 2019, 40(4): 434-447.
[5]	陈红汉, 米立军, 刘妍鷨, 韩晋阳, 孔令涛. 珠江口盆地深水区CO₂成因、分布规律与风险带预测[J]. 石油学报, 2017, 38(2): 119-134.
[6]	陈东旭, 章凤奇, 陈汉林, 杨树锋, 曹婷, 蒙启安. 新生代辉绿岩岩体识别及油气地质意义——以中国东北地区方正断陷为例[J]. 石油学报, 2016, 37(6): 757-767.
[7]	白冰, 王清斌, 赵国祥, 刘晓健. 蓬莱9-1构造新生代构造演化:磷灰石裂变径迹证据[J]. 石油学报, 2015, 36(9): 1098-1107.
[8]	张功成, 屈红军, 刘世翔, 谢晓军, 赵钊, 沈怀磊. 边缘海构造旋回控制南海深水区油气成藏[J]. 石油学报, 2015, 36(5): 533-545.
[9]	张功成, 米立军, 屈红军, 张厚和, 谢晓军, 胡圣标, 张义娜. 中国海域深水区油气地质[J]. 石油学报, 2013, 34(增刊二): 1-14.
[10]	曾清波, 吴景富, 赵志刚, 纪沫, 赵钊. 珠江口盆地白云—荔湾深水区珠江组大型水道体系的发现与勘探意义[J]. 石油学报, 2013, 34(增刊二): 48-56.
[11]	岳军培, 张艳, 沈怀磊, 尤龙, 鲁宝亮, 王璞珺. 华南陆缘地质特征对南海北部盆地基底的约束[J]. 石油学报, 2013, 34(增刊二): 120-128.
[12]	唐　永　梅廉夫　肖安成　陈友智　罗开平 . 川东北宣汉-达县地区晚中生代-新生代构造应力场转化及其油气意义[J]. 石油学报, 2013, 34(1): 59-70.
[13]	程晓敢雷刚林陈汉林杜治利廖林罗俊成师骏. 西昆仑山前甫沙—克里阳地区新生代变形特征及油气控制作用[J]. 石油学报, 2011, 32(1): 83-89.
[14]	祁鹏任建业史双双卢刚臣. 歧口凹陷沿岸带新生代构造特征及其形成机制[J]. 石油学报, 2010, 31(6): 900-905.
[15]	朱伟林. 南海北部深水区油气地质特征[J]. 石油学报, 2010, 31(4): 521-527.