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孙吴-嘉荫盆地东部太平林场组沉积相及烃源岩特征

姚玉来 李士超 杨建国 肖飞 李昂 黄一鸣 张渝金

地质与资源2023,Vol.32Issue(6):713-719,7.
地质与资源2023,Vol.32Issue(6):713-719,7.DOI:10.13686/j.cnki.dzyzy.2023.06.008

孙吴-嘉荫盆地东部太平林场组沉积相及烃源岩特征

SEDIMENTARY FACIES AND SOURCE ROCK CHARACTERISTICS OF TAIPINGLINCHANG FORMATION IN EASTERN SUNWU-JIAYIN BASIN

姚玉来 1李士超 1杨建国 1肖飞 1李昂 1黄一鸣 1张渝金1

作者信息

  • 1. 中国地质调查局 沈阳地质调查中心(东北地质科技创新中心),辽宁沈阳 110034
  • 折叠

摘要

Abstract

The Upper Cretaceous Taipinglinchang Formation is the key oil-gas exploration horizon in Sunwu-Jiayin Basin.Based on the detailed field observation and description,the sedimentology of section of Taipinglinchang Formation in the east of the basin is studied in this paper.The results show that the sedimentary facies developed in Taipinglinchang Formation include lacustrine facies and fan delta facies,which can be further divided into 3 sedimentary subfacies with 6 sedimentary microfacies.The petrology and organic geochemical characteristics of the shale in Taipinglinchang Formation are analyzed by various organic geochemical testing methods.The results indicate that the mineral composition of shale is mainly quartz,belonging to felsic shale.The maceral composition is dominated by sapropelinite,with oil-prone property.The source rocks are of medium-good quality,with the organic matter types ofⅡ1-Ⅱ2,which are in the low mature-mature stage,suggesting a good hydrocarbon potential.The results may provide basic data for further research and oil-gas exploration in the basin.

关键词

孙吴-嘉荫盆地/太平林场组/沉积相/烃源岩/黑龙江省

Key words

Sunwu-Jiayin Basin/Taipinglinchang Formation/sedimentary facies/source rock/Heilongjiang Province

分类

天文与地球科学

引用本文复制引用

姚玉来,李士超,杨建国,肖飞,李昂,黄一鸣,张渝金..孙吴-嘉荫盆地东部太平林场组沉积相及烃源岩特征[J].地质与资源,2023,32(6):713-719,7.

基金项目

中国地质调查局项目"东北地区地层古生物地质调查"(DD20230220) (DD20230220)

"松辽盆地北部页岩油战略调查"(DD20190114) (DD20190114)

"东北地区重要盆地多能源资源地质调查"(DD20221664). (DD20221664)

地质与资源

OACSTPCD

1671-1947

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