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渤海海域曹妃甸A构造带混积岩储层白云岩化成因机理分析

赵珂 宋章强 杜学斌 叶茂松 解习农 徐伟

石油实验地质2018,Vol.40Issue(2):218-225,8.
石油实验地质2018,Vol.40Issue(2):218-225,8.DOI:10.11781/sysydz201802218

渤海海域曹妃甸A构造带混积岩储层白云岩化成因机理分析

Dolomitization genetic mechanism of carbonate-siliciclastic mixed rock reservoir in CFD-A Tectonic Belt, Bohai Sea

赵珂 1宋章强 2杜学斌 1叶茂松 3解习农 1徐伟3

作者信息

  • 1. 中国地质大学 海洋学院,武汉430074
  • 2. 中海石油(中国)有限公司 天津分公司,天津300452
  • 3. 中国地质大学(武汉)构造与油气资源教育部重点实验室,武汉430074
  • 折叠

摘要

Abstract

The mixed rock is a rock that consists of a mixed deposition of siliciclastic and carbonate.It was dominated by biogenic carbonate in the CFD-A tectonic belt in the Bohai Sea where dolomitization was found. Research on the CFD-A tectonic belt was rarely reported,especially aiming at the genetic mechanism of dolomite reservoir. Based on the observation and identification of cores and rock slices,combined with a number of geochemical tests,the charac-teristics and genetic mechanism of dolomitization in mixed rocks in the first and second members of Shahejie Formation at the CFD-A tectonic belt were studied.Four dolomite types were identified:dolomicrite,bioclastic-containing dolo-micrite,bioclastic dolomite and sand-containing bioclastic dolomite. Further analyses showed that negative bias and positive correlation were both found in carbon and oxygen stable isotopes. Dispersed distribution and large variation were also revealed in oxygen stable isotopes. Dolomitization was found only in bioclastic and its ring cement through microscopic photos,which did not occur in interlocking cementation and bioclast filling.Lake surface fluctuation can be revealed by Mn/Fe,Sr/Ba index,indicating that the tectonic belt has suffered from fresh water leaching because of exposure.Mixed water dolomitization is the dominated genetic mechanism of dolomites in the study area.

关键词

成因机理/地球化学/储层/白云岩/沙河街组/曹妃甸A构造带/渤海海域

Key words

genetic mechanism/geochemistry/reservoir/dolomite/Shahejie Formation/CFD⁃A tectonic belt/Bohai Sea

分类

能源科技

引用本文复制引用

赵珂,宋章强,杜学斌,叶茂松,解习农,徐伟..渤海海域曹妃甸A构造带混积岩储层白云岩化成因机理分析[J].石油实验地质,2018,40(2):218-225,8.

基金项目

国家自然科学基金项目(41772111)和国家重点基础研究发展计划(973计划)项目(2017CB239102)资助. (41772111)

石油实验地质

OA北大核心CSCDCSTPCD

1001-6112

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