珠江口盆地恩平凹陷珠琼运动二幕的构造—沉积响应及区域构造意义

doi:10.7623/syxb201104005

石油学报 ›› 2011, Vol. 32 ›› Issue (4): 588-595.DOI: 10.7623/syxb201104005

珠江口盆地恩平凹陷珠琼运动二幕的构造—沉积响应及区域构造意义

王家豪 1,2 刘丽华 3 陈胜红 3 尚亚乐 1

1中国地质大学资源学院湖北武汉 430074； 2中国地质大学构造与油气资源教育部重点实验室湖北武汉 430074； 3中海石油（中国）有限公司深圳分公司广东广州 510240

收稿日期:2010-11-27 修回日期:2011-03-18 出版日期:2011-07-25 发布日期:2011-09-22
通讯作者: 王家豪
作者简介:王家豪，男，1968年10月生，2005年获中国地质大学（武汉）博士学位，现为中国地质大学（武汉）副教授，主要从事沉积学、层序地层学方面的研究工作。
基金资助:
国家自然科学基金项目（No.40872077）资助。

Tectonic-sedimentary responses to the second episode of the Zhu-Qiong movement in the Enping Depression, Pearl River Mouth Basin and its regional tectonic significance

WANG Jiahao 1,2 LIU Lihua 3 CHEN Shenghong 3 SHANG Yale 1

Received:2010-11-27 Revised:2011-03-18 Online:2011-07-25 Published:2011-09-22

摘要/Abstract

摘要：

珠琼运动二幕是发生在珠江口盆地晚始新世—早渐新世的一次重大构造运动。通过对恩平凹陷的地震层序、沉积演化和断裂活动研究揭示，珠琼运动二幕的构造—沉积响应表现为文昌组与恩平组之间的区域性不整合面、盆地演化从断陷至断—拗阶段的变革、沉降中心迁移、新生EW走向断层和沉积体系整体转变等。结合中国东部渤海湾盆地黄骅坳陷的研究，珠琼运动二幕及同期构造作用不仅在珠江口盆地，而且在中国东部新生代盆地均可追索，对盆地构造演化、沉积充填以及油气生-储-盖组合均产生了重要影响，其共同特点是拗陷作用增强、区域应力场顺时针方向偏转并伴随右旋张扭作用，其形成与晚始新世以来印度板块与欧亚板块碰撞作用有关。

关键词: 珠江口盆地, 恩平凹陷, 古近纪, 珠琼运动, 层序地层

Abstract:

The second episode of the Zhu-Qiong movement is an important tectonic event that occurred from late Eocene to early Oligocene in the Pearl River Mouth Basin. Studies on seismic stratigraphic sequences, depositional evolution and fault activities of the Enping Depression have revealed that tectonic and sedimentary responses to the second episode of the Zhu-Qiong movement are characterized by a regional unconformity between the Enping Formation and the underlying Wenchang Formation, evolutional transform of the basin from rift to fault sag; migration of subsidence centers, generation of EW-orientated faults and the whole transform of depositional system. Furthermore, integrated with studies on the Huanghua Depression of the Bohai Bay Basin, eastern China, it has been proposed that the second episode of the Zhu-Qiong movement and its synchronous tectonism can be found not only in the Pearl River Mouth Basin but also in other Cenozoic basins of eastern China, they have affected tectonic evolution, deposition, and petroleum system of these basins greatly. These effects are commonly characterized by strengthening of downwarping and dextrorotatory deflection of regional stress fields with dextrorotatory tense-shearing action, and generally resulted from the collision of the Indian Plate with the Eurasian Plate since late Eocene.

Key words: Pearl River Mouth Basin, Enping Depression, Paleogene, Zhu-Qiong movement, stratigraphic sequence

王家豪刘丽华陈胜红尚亚乐. 珠江口盆地恩平凹陷珠琼运动二幕的构造—沉积响应及区域构造意义[J]. 石油学报, 2011, 32(4): 588-595.

WANG Jiahao LIU Lihua CHEN Shenghong SHANG Yale. Tectonic-sedimentary responses to the second episode of the Zhu-Qiong movement in the Enping Depression, Pearl River Mouth Basin and its regional tectonic significance[J]. Editorial office of ACTA PETROLEI SINICA, 2011, 32(4): 588-595.

参考文献

[1]陈长民,施和生,许仕策,等.珠江口盆地(东部) 第三系油气藏形成条件[M].北京:科学出版社,2003：1-87.

Chen Changmin,Shi Hesheng,Xu Shice,et al.The condition of hydrocarbon accumulation of Tertiary petroleum system in Pearl River Mouth Basin [M].Beijing：Science Press,2003：1-87.

[2]焦养泉,李思田,解习农,等.多幕裂陷作用的表现形式——以珠江口盆地西部及其外围地区为例[J].石油实验地质,1997, 19(3): 222-227.

Jiao Yangquan,Li Sitian,Xie Xinong,et al.Manifestation of multistage episodic rifting:Taking western Pearl River Mouth Basin and its peripheral area as an example [J].Experimental Petroleum Geology,1997,19(3):222-227.

[3]崔莎莎,何家雄,陈胜红,等.珠江口盆地发育演化特征及其油气成藏地质条件[J].天然气地球科学,2009,20(3):384-391.

Cui Shasha,He Jiaxiong,Chen Shenghong,et al.Development characteristics of Pearl River Mouth Basin and its geological conditions for oil and gas accumulation [J].Natural Gas Geoscience,2009,20(3):384-391.

[4]任建业.渤海湾盆地东营凹陷S6’界面的构造变革意义[J].地球科学,2004,29(1):69-76.

Ren Jianye.Tectonic significance of S6’ boundary in Dongying Depression,Bohai Gulf Basin [J].Earth Science,2004,29(1): 69-76.[5]米立军,张功成,沈怀磊,等.珠江口盆地深水区白云凹陷始新统—下渐新统沉积特征[J].石油学报,2008,29(1):29-34.

Mi Lijun,Zhang Gongcheng,Shen Huailei,et al.Eocene-Lower Oligocene sedimentation characteristics of Baiyun Sag in the deep water area of Pearl River Mouth Basin [J].Acta Petrolei Sinica,2008,29(1):29-34.

[6]施和生,于水明,梅廉夫,等.珠江口盆地惠州凹陷古近纪幕式裂陷特征[J].天然气工业,2009,29(1):34-40.

Shi Hesheng,Yu Shuiming,Mei Lianfu,et al.Features of Paleogene episodic rifting in Huizhou fault depression in the Pearl River Mouth Basin [J].Natural Gas Industry,2009,29(1):34-40.

[7]陈国俊,吕成福,李玉兰,等.珠江口盆地恩平凹陷文昌组浊积体含油气性分析[J].沉积学报,2008,26 (5):881-885.

Chen Guojun,Lü Chengfu,Li Yulan,et al.Analysis of the oil and gas-bearing turbidite within Wenchang Formation in Enping Depression,Pearl River Mouth Basin,China [J].Acta Sedimentologica Sinica,2008,26 (5):881-885.

[8]李友川,陶维祥,孙玉梅,等.珠江口盆地惠州凹陷及其邻区原油分类和分布特征[J].石油学报,2009,30(6):830-834.

Li Youchuan,Tao Weixiang,Sun Yumei,et al.Classification and distribution of oil in Huizhou Depression of Pearl River Mouth Basin [J].Acta Petrolei Sinica,2009,30(6):830-834.

[9]陈汉宗,吴湘杰,周蒂,等.珠江口盆地中新生代主要断裂特征和动力背景分析[J].热带海洋学报,2005,24(2):52-59.

Chen Hanzong,Wu Xiangjie,Zhou Di,et al.Meso-Cenozoic faults in Zhujiang River Mouth Basin and their geodynamic background [J].Journal of Tropical Oceanography,2005,24(2):52-59.

[10]Ru Ke,Pigott S D.Episodic rifting and subsidence in the South China Sea [J].AAPG Bulletin,1986,70(9):1136-1155.

[11]蔡周荣,刘维亮,万志峰,等.南海北部新生代构造运动厘定及与油气成藏关系探讨[J].海洋通报,2010,29(2):161-165.

Cai Zhourong,Liu Weiliang,Wan Zhifeng,et al.Determination of Cenozoic tectonic movement in the northern South China Sea and the relationship between oil-gas reservoir and tectonic movement [J].Marine Science Bulletin,2010,29(2):161-165.

[12]王家豪,王华,肖敦清,等.陆相伸展性盆地二级层序的厘定[J].石油学报,2009,30(6):869-875.

Wang Jiahao,Wang Hua,Xiao Dunqing,et al.Determination of second-order stratigraphic sequences in continental extensional basins [J].Acta Petrolei Sinica,2009,30(6):869-875.

[13]冯有良,周海民,任建业,等.渤海湾盆地东部古近系层序地层及其对构造活动的响应[J].中国科学D辑：地球科学,2010,40(10):1356-1376.

Feng Youliang,Zhou Haimin,Ren Jianye,et al.Paleogene sequence stratigraphy in the east of the Bohai Bay Basin and its response to structural movement[J].Sci.Sin.Terrae,2010,40(10):1356-1376.

[14]佟殿君,任建业,史双双,等.黄骅坳陷新生代关键性构造运动面的确定及盆地演化过程[J].油气地质与采收率,2010,17(2): 9-13.

Tong Dianjun,Ren Jianye,Shi Shuangshuang,et al.Determination on key tectonic movement surfaces and analysis on evolution process of Huanghua Depression [J].Petroleum Geology and Recovery Efficiency,2010,17(2):9-13.

[15]王华,廖远涛,陆永潮,等.中国东部新生代陆相断陷盆地层序的构成样式[J].中南大学学报:自然科学版,2010,41(1):277-285.

Wang Hua,Liao Yuantao,Lu Yongchao,et al.Sequence architecture styles of Cenozoic continental rift basins in East China [J].Journal of Central South University:Science and Technology,2010,41(1):277-285.

[16]池英柳,赵文智.渤海湾盆地新生代走滑构造与油气聚集[J].石油学报,2000,21(2):14-20.

Chi Yingliu,Zhao Wenzhi.Strike-slip deformation during the Cenozoic and its influence on hydrocarbon accumulation in the Bohai Bay Basin [J].Acta Petrolei Sinica,2000,21(2):14-20.

[17]漆家福.渤海湾新生代盆地的两种构造系统及其成因解释[J].中国地质,2004,31(1):15-21.

Qi Jiafu.Two tectonic systems in the Cenozoic Bohai Bay basin and their genetic interpretation [J].Geology in China,2004, 31(1): 15-21.

[18]Zhou D,Ru K,Chen H Z.Kinematics of Cenozoic extension on the South China Sea continental margin and its implications for the tectonic evolution of the region [J].Tectonophysics,1995,251:161-177.

[19]Zhou Jiangyu,Wang Jianghai,Brian K H,et al.Sedimentology and chronology of Paleogene coarse clastic rocks in east-central Tibet and their relationship to early tectonic uplift [J].Acta Geologica Sinica,2007,81(3):398-408.

珠江口盆地恩平凹陷珠琼运动二幕的构造—沉积响应及区域构造意义

Tectonic-sedimentary responses to the second episode of the Zhu-Qiong movement in the Enping Depression, Pearl River Mouth Basin and its regional tectonic significance

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]	高阳东, 刘军, 彭光荣, 陈林, 王梓颐, 史玉玲. 珠江口盆地油气勘探新领域及资源潜力[J]. 石油学报, 2024, 45(1): 183-201.
[2]	朱筱敏, 王华, 朱红涛, 邵龙义, 纪友亮. 陆相层序地层学研究进展及发展关注[J]. 石油学报, 2023, 44(8): 1382-1398.
[3]	高阳东, 彭光荣, 陈兆明, 姜大朋, 马宁, 李潇, 吕华星, 高中亮. 珠江口盆地开平凹陷深水古近系勘探重大发现及意义[J]. 石油学报, 2023, 44(7): 1029-1040.
[4]	彭光荣, 郭婧, 姜福杰, 姜大朋, 吴宇琦, 陈兆明, 宋泽章, 高中亮, 张宇琦. 珠江口盆地开平凹陷烃源岩地球化学特征与油源对比[J]. 石油学报, 2023, 44(10): 1624-1636.
[5]	杨雪, 石学文, 朱逸青, 刘佳, 李怡, 何亮, 徐亮, 李彦佑, 陈瑶, 蒋佳玉. 四川盆地南部泸州地区凯迪阶—埃隆阶深水页岩沉积演化与有机质富集[J]. 石油学报, 2022, 43(4): 469-482.
[6]	张向涛, 李军, 向绪洪, 赵靖舟. 珠江口盆地深水区白云凹陷超压成因机制及其勘探意义[J]. 石油学报, 2022, 43(1): 41-57.
[7]	谢环羽, 姜在兴, 王培玺, 谢武仁, 杨雨. 中—上扬子地区寒武系层序地层格架[J]. 石油学报, 2021, 42(7): 865-884.
[8]	张向涛, 李小平, 玄昌姬, 杜家元, 丁琳, 李智高, 陈维涛. 南海东部浅水区非烃源岩层系岩性油藏勘探实践与方向[J]. 石油学报, 2021, 42(6): 695-707.
[9]	米立军, 张向涛, 庞雄, 郑金云, 张丽丽. 珠江口盆地形成机制与油气地质[J]. 石油学报, 2019, 40(s1): 1-10.
[10]	杨计海, 杨希冰, 游君君, 江汝锋, 徐涛, 胡高伟, 李珊珊, 陈林. 珠江口盆地珠三坳陷油气成藏规律及勘探方向[J]. 石油学报, 2019, 40(s1): 11-25.
[11]	柳广弟, 牛子铖, 陈哲龙, 张向涛, 雷永昌, 张梦媛, 王小龙, 汪旭东. 珠江口盆地陆丰凹陷在洼陷迁移控制下的油气成藏规律[J]. 石油学报, 2019, 40(s1): 26-40,216.
[12]	代一丁, 牛子铖, 汪旭东, 王小龙, 肖张波, 张凯迪, 赵璇. 珠江口盆地陆丰凹陷古近系与新近系油气富集规律的差异及其主控因素[J]. 石油学报, 2019, 40(s1): 41-52.
[13]	朱明, 张向涛, 黄玉平, 朱俊章, 龙祖烈, 史玉玲, 石创, 张小龙. 珠江口盆地烃源岩特征及资源潜力[J]. 石油学报, 2019, 40(s1): 53-68.
[14]	朱筱敏, 葛家旺, 吴陈冰洁, 张向涛, 汪旭东, 李晓燕, 黎明. 珠江口盆地陆丰凹陷深层砂岩储层特征及主控因素[J]. 石油学报, 2019, 40(s1): 69-80.
[15]	罗静兰, 何敏, 庞雄, 李弛, 柳保军, 雷川, 马永坤, 庞江. 珠江口盆地南部热演化事件与高地温梯度的成岩响应及其对油气勘探的启示[J]. 石油学报, 2019, 40(s1): 90-104.