北黄海盆地新近纪以来断裂特征及对古近纪断裂的继承性
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摘要
新近纪以来构造运动对油气成藏的作用越来越受到重视,为了增加对北黄海新近纪以来地质和构造特征的了解,利用新近获得的覆盖大部分北黄海海域的地震资料以及船测重力资料,识别出北黄海海域新近纪以来的主要断层,发现它们主要为正断层.绝大部分主要断层在剖面上显示出"半地堑"边界断层的特点,在隆起带上也发育新近纪-第四纪断层,对应了重力异常条带的边界;此外,也有一些断层显示出明显的走滑特点,如北黄海西缘断裂.对比古近纪断裂图,发现在盆地内,这些新近纪断层是古近纪断层的继承,但因隆起带上缺少古近纪断层资料目前还未能判断继承性.
The role of the Neogene tectonic movements to the hydrocarbon accumulation has been paid more attention these years.To the better understanding of the Neogene geology and structural pattern of the North Yellow Sea basin,we identify main Neogene-Quaternary(N-Q)faults by interpreting the newly-acquired seismic data and ship borne gravity data.Most of the interpreted faults are boundary normal faults of the depressions within the basin and in the uplifts.Besides,some faults possess the characteristics of the strike-slip fault,e.g.the west-marginal North Yellow Sea fault.Compared with Paleogene faults,we find that the N-Q faults are inherited to the Paleogene faults within the basin,but it is difficult to determine the inheritance of the N-Q faults to the Paleogene ones in the upliftsbecause of the lack of the Paleogene fault data in the uplifts.
引文
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