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首页|期刊导航|地质科学|塔里木盆地麦盖提斜坡西段成藏演化与有利勘探区域:以巴什托普油田为例

塔里木盆地麦盖提斜坡西段成藏演化与有利勘探区域:以巴什托普油田为例

陈秀艳 孙崇浩 陶小晚 李洪辉 杜德道 王珊 闫磊 王斌

地质科学2024,Vol.59Issue(4):991-1002,12.
地质科学2024,Vol.59Issue(4):991-1002,12.DOI:10.12017/dzkx.2024.070

塔里木盆地麦盖提斜坡西段成藏演化与有利勘探区域:以巴什托普油田为例

Hydrocarbon accumulation and favorable exploration areas in the western Maigaiti slope of Tarim Basin:A case study of Bashituopu oilfield

陈秀艳 1孙崇浩 2陶小晚 1李洪辉 1杜德道 1王珊 1闫磊 1王斌2

作者信息

  • 1. 中国石油天然气股份有限公司勘探开发研究院 北京 100083
  • 2. 中国石油天然气股份有限公司塔里木油田分公司 新疆库尔勒 841000
  • 折叠

摘要

Abstract

The strata above and below the Middle Cambrian salt are the current research and exploration hotspots in the Maigaiti slope,Tarim Basin.The fracture characteristics were analyzed on the basis of seismic interpretation.Combined with the study results of structural geology,sedimentology and the thermal evolution history,the accumulation history of Bashituopu oilfield was analyzed.The Caledonian hydrocarbon migration and accumulation mainly occurred below the Cambrian salt at the western Maigaiti slope from north to south.Oil-gas migrated vertical upwards through northwestward strike-slip faults in the north and south sides of Bashituopu oilfield,and accumulated at the Bashituopu anticline forming an ancient oil reservoir in Hercynian Period.The present residual Bashituopu reservoir was formed in the Himalayan Period,besides the oil-gas adjusted from west to east,a small amount of lateral oil-gas filling.Both strike-slip fractures at the north and south sides of Bashituopu oilfield and traps under the Bashituopu main detachment faults are the favorable exploration objectives in the western segment of Maigaiti slope.

关键词

盐上/盐下/断裂作用/储层沥青/流体包裹体/成藏演化/勘探区域

Key words

Sub-salt strata/Above-salt strata/Rifting/Reservoir asphalt/Fluid inclusion/Accumulation history/Favorable areas of petroleum exploration

分类

天文与地球科学

引用本文复制引用

陈秀艳,孙崇浩,陶小晚,李洪辉,杜德道,王珊,闫磊,王斌..塔里木盆地麦盖提斜坡西段成藏演化与有利勘探区域:以巴什托普油田为例[J].地质科学,2024,59(4):991-1002,12.

基金项目

中国石油股份科技项目(编号:2021DJ0502)资助 (编号:2021DJ0502)

地质科学

OA北大核心CSTPCD

0563-5020

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