首页|基于成像测井的西湖凹陷古近系花港组及平湖组物源分析

基于成像测井的西湖凹陷古近系花港组及平湖组物源分析

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沉积物源分析对沉积相图编制以及开发方案设计意义重大.本文以西湖凹陷区域宏观、微观地质资料研究为基础,利用成像测井资料进行岩性识别、沉积构造拾取、沉积微相研究以及古水流方向分析,进而对凹陷内两个区带、两个层系的物源进行分析,结果认为中央带渐新统花港组物源以东北部虎皮礁隆起的变质母岩为主,物源区长距离轴向搬运沉积,物源区较为稳定.平湖斜坡带平北区始新统平湖组物源以西部海礁隆起的岩浆母岩为主,并以短源运输沉积为主,平面上相带变化较快.研究成果对于西湖凹陷平湖组沉积相认识、砂体展布等研究具有指导意义.
Provenance analysis of Huagang Formation of central belt and Pinghu Formation of Pingbei area in Xihu sag based on image logging
This article is based on the study of macro and micro geological data in the Xihu sag.It utilizes image logging data for lithology,lithofacies,sedimentary facies,and microfacies identification,as well as the analysis of paleocurrent direction.Subsequently,it analyzes the provenance of two zones and two series of strata in Xihu sag,concluding that the provenance area of the Oligocene Huagang Formation in the middle zone is dominated by metamorphic parent rocks from Hupijiao uplift in the northeast,with long-range axial transported deposition,and it is relatively stable;the provenance area of Eocene Pinhu Formation in Pinghu slope zone is dominated by magmatic parent rocks from Haijiao uplift in the west,with short-rang transported deposition,and the facies zone changes quickly on the plane.

Image logsPaleocurrent directionProvenanceHuagang FormationPinghu Formation

何玉春、何志斌、李帅、张国栋、鲁法伟、赖锦、蔡军

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中海石油(中国)有限公司上海分公司,上海 200335

中国石油大学(北京)地球科学学院,北京 102249

成像测井 古水流 物源 花港组 平湖组

中海石油(中国)有限公司重大专项

2024

地球物理学进展
中国科学院地质与地球物理研究所 中国地球物理学会

地球物理学进展

CSTPCD北大核心
影响因子:1.761
ISSN:1004-2903
年,卷(期):2024.39(2)