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北羌塘胜利河地区布曲组优质烃源岩形成环境与有机质富集机制

陈程 吴珍汉 赵为永 王利 季长军 赵珍 张浩 龚赞

地质学报2024,Vol.98Issue(2):530-543,14.
地质学报2024,Vol.98Issue(2):530-543,14.DOI:10.19762/j.cnki.dizhixuebao.2023262

北羌塘胜利河地区布曲组优质烃源岩形成环境与有机质富集机制

Formation environment and organic matter enrichment mechanism of high-quality source rocks in the Buqu Formation in the Shenglihe area,northern Qiangtang basin

陈程 1吴珍汉 2赵为永 3王利 4季长军 2赵珍 2张浩 1龚赞5

作者信息

  • 1. 中国地质科学院地质力学研究所,北京,100081||自然资源部古地磁与古构造重建重点实验室,北京,100081||中国地质调查局油气地质力学重点实验室,北京,100081
  • 2. 中国地质科学院,北京,100037
  • 3. 中国石油青海油田分公司勘探开发研究院,甘肃敦煌,736202
  • 4. 中国地质调查局,北京,100037
  • 5. 中国地质调查局南京地质调查中心,江苏南京,210016
  • 折叠

摘要

Abstract

The Qiangtang basin is the Mesozoic marine sedimentary basin with the lowest degree of oil and gas exploration in the new land area,and its main source rocks have not been clearly understood.In this paper,the organic geochemistry and element geochemistry of the source rocks of the Middle Jurassic Buqu Formation in Shenglhe area have been systematically studied,and the formation environment and organic matter enrichment mechanism of the source rocks of the Buqu Formation have been discussed.This provides a theoretical basis for predicting the distribution of high-quality source rocks in the Middle Jurassic Buqu Formation in the North Qiangtang depression.The source rocks of the Buqu Formation in Shenglihe area have high abundance of type Ⅱ of organic matter in mature stage.During the Buqu period,the climate was arid and hot,and the primary productivity level of the study area was relatively high,which was a weakly confined basin with shallow water,high salinity and oxygen-poor depositional environment.During the Buqu period,large-scale transgression occurred in the Qiangtang basin,and the study area was adjacent to the central uplift.A large number of nutrients such as phosphorus and iron from terrigenous input and hydrothermal activities were carried into the ocean,resulting in higher primary productivity,which was the main controlling factor for the enrichment of organic matter in high-quality source rocks of the Buqu Formation in the North Qiangtang depression.The study area is located in the minimum oxygen-containing zone of the North Qiangtang depression,which is conducive to the anoxic death and burial of a large number of planktons.Through the analysis of organic matter enrichment mechanism,the coastal shelf slope zone of the North Qiangtang depression may be a favorable area for the distribution of high-quality source rocks in the Middle Jurassic Buqu Formation.

关键词

有机质富集/优质烃源岩/古生产力/胜利河/北羌塘坳陷

Key words

organic matter enrichment/high-quality source rock/palaeoproductivity/Shenglihe area/northern Qiangtang basin

引用本文复制引用

陈程,吴珍汉,赵为永,王利,季长军,赵珍,张浩,龚赞..北羌塘胜利河地区布曲组优质烃源岩形成环境与有机质富集机制[J].地质学报,2024,98(2):530-543,14.

基金项目

本文为国家自然科学基金项目(编号 42102201)和中国地质调查项目(编号 DD20221660-2)联合资助的成果. (编号 42102201)

地质学报

OA北大核心CSTPCD

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