Formation of Liaodong uplift and collapse of the ancient Liaozhong sag in Tan-Lu fault zone

doi:10.7623/syxb201503003

Acta Petrolei Sinica ›› 2015, Vol. 36 ›› Issue (3): 274-285.DOI: 10.7623/syxb201503003

• Petroleum Exploration • Previous Articles Next Articles

Formation of Liaodong uplift and collapse of the ancient Liaozhong sag in Tan-Lu fault zone

Peng Jingsong¹, Xu Changgui¹, Wu Kui¹, Huang Xiaobo¹, Zhang Rucai¹, Deng Jun¹, Liu Yongjun1, Yu Yixin²

1. Tianjin Branch,CNOOC China Limited, Tianjin 300452, China;
2. Key Laboratory of Hydrocarbon Accumulation Mechanism of the Ministry of Education, China University of Petroleum, Beijing 102249, China

Received:2014-07-28 Revised:2014-11-18 Online:2015-03-25 Published:2015-03-11

郯庐断裂带辽东凸起的形成与古辽中洼陷的瓦解

彭靖淞¹, 徐长贵¹, 吴奎¹, 黄晓波¹, 张如才¹, 邓君¹, 柳永军¹, 余一欣²

1. 中海石油(中国)有限公司天津分公司天津 300452;
2. 中国石油大学石油天然气成藏机理教育部重点实验室北京 102249

通讯作者: 彭靖淞,男,1984年4月生,2006年获成都理工大学学士学位,2009年获成都理工大学硕士学位,现为中海石油(中国)有限公司天津分公司渤海石油研究院勘探地质工程师,主要从事石油地质综合研究工作。Email:pengjs@cnooc.com.cn
作者简介:彭靖淞,男,1984年4月生,2006年获成都理工大学学士学位,2009年获成都理工大学硕士学位,现为中海石油(中国)有限公司天津分公司渤海石油研究院勘探地质工程师,主要从事石油地质综合研究工作。Email:pengjs@cnooc.com.cn
基金资助:
国家重大科技专项"近海大中型油气田形成条件与分布"(2011ZX05023-006)资助

Abstract

Abstract:

Liaodong uplift is located in the northern Bohai part of Tan-Lu fault zone, adjacent to the west of Liaozhong sag. The tectonic evolution of Liaodong uplift is extremely complicated as influenced by the double dynamic source and multi-stage episodic activities of Tan-Lu fault zone since the Cenozoic. In particular, the formation period of Liaodong uplift has still not been determined. Aiming at this issue, based on new theories and techniques in tectonic geology (fault-related fold theory and sandbox simulation experiment), this study proposes that the strike-slip inversion structure of Liaodong uplift had begun to develop from the depositional stage of the third member of Dongying Formation (30.3 Ma), which is demonstrated in terms of the marginal fracture system evolution, stratigraphic distribution, axial surface inflection point of normal drag folds, unconformity distribution as well as slump and sublacustrine fans. Further, the existence and collapse of the "ancient Liaozhong sag" is first presented herein through tectonic evolution analysis, based on which it is explored using sandbox simulation experiment that the partial and intense differential settlement caused by oblique pull-apart and strike-slip activities is contributed to the "relative uplift" of Liaodong.

Key words: Tan-Lu fault, strike-slip, normal drag folds, ancient Liaozhong sag, collapse

摘要：

辽东凸起位于郯庐断裂渤海段的北部,西邻辽中洼陷,受新生代以来郯庐断裂带双动力源和多期次幕式活动的影响,其构造演化非常复杂,特别是辽东凸起的形成时间一直未有定论。为了解决这个问题,根据构造地质学新理论和方法(断层相关褶皱和沙箱模拟),通过辽东凸起周缘断裂系统变革、地层分布、正牵引褶皱轴面变化、不整合分布和滑塌湖底扇等方面论证了辽东凸起在东营组三段沉积末期(30.3Ma)开始反转形成,并依据构造演化首次提出了"大古辽中洼陷"的存在及其瓦解。在此基础上,结合沙箱模拟实验探讨了郯庐断裂斜向拉分及其走滑活动产生了局部范围内剧烈的差异沉降促成辽东凸起的"相对隆升"。

关键词: 郯庐断裂, 走滑, 正牵引褶皱, 古辽中洼陷, 瓦解

Peng Jingsong, Xu Changgui, Wu Kui, Huang Xiaobo, Zhang Rucai, Deng Jun, Liu Yongjun, Yu Yixin. Formation of Liaodong uplift and collapse of the ancient Liaozhong sag in Tan-Lu fault zone[J]. Acta Petrolei Sinica, 2015, 36(3): 274-285.

彭靖淞, 徐长贵, 吴奎, 黄晓波, 张如才, 邓君, 柳永军, 余一欣. 郯庐断裂带辽东凸起的形成与古辽中洼陷的瓦解[J]. 石油学报, 2015, 36(3): 274-285.

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Formation of Liaodong uplift and collapse of the ancient Liaozhong sag in Tan-Lu fault zone

郯庐断裂带辽东凸起的形成与古辽中洼陷的瓦解

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