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塔里木盆地巴楚—麦盖提地区古构造迁移特征及其意义

王斌 王祥 程晓敢 李洪辉 能源 吕惠贤 屈洋 阿里木·卡德尔

地质科学2018,Vol.53Issue(1):133-145,13.
地质科学2018,Vol.53Issue(1):133-145,13.DOI:10.12017/dzkx.2017.008

塔里木盆地巴楚—麦盖提地区古构造迁移特征及其意义

Significance and characteristics of paleotectonic migration in Bachu-Makit area of Tarim Basin

王斌 1王祥 1程晓敢 2李洪辉 3能源 1吕惠贤 1屈洋 1阿里木·卡德尔4

作者信息

  • 1. 中国石油塔里木油田分公司勘探开发研究院 新疆库尔勒841000
  • 2. 浙江大学地球科学学院 杭州310027
  • 3. 中国石油勘探开发研究院 北京 100083
  • 4. 中国石油塔里木油田分公司开发事业部 新疆库尔勒841000
  • 折叠

摘要

Abstract

The Bachu-Meigeti area in the Tarim Basin experienced multi-period tectonic movement.It is of great significance to reconstruct the tectonic evolution of the area and to guide the exploration of oil and gas,which depicts accurately the shape and migration characteristics of the paleotectonic.Combined with geological and geophysical studies,applying the thickness map method to reflect the palaeotectonic of the upper boundary of the Lower Cambrian in the Bachu-Meigeti area,and discuss its migration process.And the vertical tectonic variation intensity method is used to quantitatively calculate the tectonic activity degree of the study area.The results show that:1) In the west of the study area,there is a large-scale migration of paleotectonic,while the eastern part is relatively stable.2) There is relatively stable of tectonic activity during Caledonian-Early Himalayan period,and strong in Late Himalayan period.A multi-stage relatively inactive zone is developed along the Maketi slope.3) The Lower Cambrian dolomite in the eastern Maketi slope is characterized by relatively low activity intensity,and a higher structural position relative to the hydrocarbon generation depression,which is the favorable objective area for the migration and accumulation of oil and gas.

关键词

古构造迁移/构造活动强度/构造变动强度/下寒武统/巴楚—麦盖提地区

Key words

Palaeotectonic migration/Tectonic activity intensity/Tectonic deformation intensity/Lower Cambrian/Bachu-Makit area

分类

天文与地球科学

引用本文复制引用

王斌,王祥,程晓敢,李洪辉,能源,吕惠贤,屈洋,阿里木·卡德尔..塔里木盆地巴楚—麦盖提地区古构造迁移特征及其意义[J].地质科学,2018,53(1):133-145,13.

基金项目

国家科技重大专项(编号:2011ZX05003-004)资助. (编号:2011ZX05003-004)

地质科学

OA北大核心CSCDCSTPCD

0563-5020

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