渤海海域428凸起地区沙一二段沉积体系及其主控因素

王启明, 杜晓峰, 加东辉, 宛良伟. 渤海海域428凸起地区沙一二段沉积体系及其主控因素[J]. 沉积与特提斯地质, 2015, 35(4): 12-16.
引用本文: 王启明, 杜晓峰, 加东辉, 宛良伟. 渤海海域428凸起地区沙一二段沉积体系及其主控因素[J]. 沉积与特提斯地质, 2015, 35(4): 12-16.
WANG Qi-ming, DU Xiao-feng, JIA Dong-hui, WAN Liang-wei. The 1st and 2nd members of the Shahejie Formation in No. 428 uplifted area,Bohai Sea: Sedimentary systems and their controlling factors[J]. Sedimentary Geology and Tethyan Geology, 2015, 35(4): 12-16.
Citation: WANG Qi-ming, DU Xiao-feng, JIA Dong-hui, WAN Liang-wei. The 1st and 2nd members of the Shahejie Formation in No. 428 uplifted area,Bohai Sea: Sedimentary systems and their controlling factors[J]. Sedimentary Geology and Tethyan Geology, 2015, 35(4): 12-16.

渤海海域428凸起地区沙一二段沉积体系及其主控因素

The 1st and 2nd members of the Shahejie Formation in No. 428 uplifted area,Bohai Sea: Sedimentary systems and their controlling factors

  • 近年的研究表明,渤海海域428凸起地区沙一二段具有良好的油气勘探前景。通过钻井、岩心、薄片、地震资料的综合分析,识别出研究区发育扇三角洲、湖泊相以及一种特殊的沉积类型——混合沉积,并对其平面分布和相互关系进行了研究。本区沉积体系的发育主要受控于物源体系、同沉积断裂样式、古地形等因素。其中,物源体系控制了砂体发育的规模,同沉积断裂样式控制了砂体的平面展布,有利的古地形条件控制了混合沉积的发育位置。
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出版历程
收稿日期:  2014-10-24
修回日期:  2015-11-29
刊出日期:  2015-12-30

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