东海西湖凹陷平湖斜坡带断裂系统特征及成因机制探讨

张建培. 东海西湖凹陷平湖斜坡带断裂系统特征及成因机制探讨[J]. 地质科学, 2013, 48(1): 291-303. doi: 10.3969/j.issn.0563-5020.2013.01.020
引用本文: 张建培. 东海西湖凹陷平湖斜坡带断裂系统特征及成因机制探讨[J]. 地质科学, 2013, 48(1): 291-303. doi: 10.3969/j.issn.0563-5020.2013.01.020
Zhang Jianpei. Fault system and its genetic mechanism in the Pinghu slope of the Xihu Sag in the East China Sea Shelf Basin[J]. Chinese Journal of Geology, 2013, 48(1): 291-303. doi: 10.3969/j.issn.0563-5020.2013.01.020
Citation: Zhang Jianpei. Fault system and its genetic mechanism in the Pinghu slope of the Xihu Sag in the East China Sea Shelf Basin[J]. Chinese Journal of Geology, 2013, 48(1): 291-303. doi: 10.3969/j.issn.0563-5020.2013.01.020

东海西湖凹陷平湖斜坡带断裂系统特征及成因机制探讨

详细信息
    作者简介:

    张建培,男,1964年8月生,硕士,高级工程师,石油地质学专业。E-mail:zhangjp918@163.com

  • 中图分类号: P542;P618.13

Fault system and its genetic mechanism in the Pinghu slope of the Xihu Sag in the East China Sea Shelf Basin

  • 综合运用地震剖面解释结果和构造编图成果,对东海西湖凹陷平湖斜坡带断裂系统按发育规模和形成期次进行分类,分析了断裂系统的平、剖面展布特征,采用古落差法和活动速率法研究了断裂运动学特征,结合区域应力场特征探讨了其成因机制。结果表明,平湖斜坡带断裂系统可划分为4个断裂带,由北至南依次为孔雀亭同向断裂带、武云亭反向断裂带、平湖同向断裂带和平南堑式断裂带。平湖斜坡带以发育多米诺、地堑、梳妆、正牵引等伸展构造样式为主,局部(如平湖同向断裂带)见微弱反转构造。断裂运动学特征研究表明,断裂活动高峰期具有分带性,平湖同向断裂带断层活动性最强,孔雀亭同向断裂带和武云亭反向断裂带次之,平南堑式断裂带最弱。平湖斜坡带断裂系统的发生、发展是应力集中与断层间相互影响共同作用的结果,是对东海陆架盆地构造演化过程的局部响应。
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出版历程
收稿日期:  2012-05-25
修回日期:  2012-10-18
刊出日期:  2013-01-25

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