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塔里木盆地轮南地区中生界断裂体系特征及成因机制

汤济广 李静 周旭 高永亮 姚嘉玮 李博文

长江大学学报(自然科学版)2024,Vol.21Issue(5):1-11,11.
长江大学学报(自然科学版)2024,Vol.21Issue(5):1-11,11.

塔里木盆地轮南地区中生界断裂体系特征及成因机制

Characteristics and genetic mechanism of Mesozoic fault system in Lunnan area,Tarim Basin

汤济广 1李静 1周旭 2高永亮 3姚嘉玮 1李博文1

作者信息

  • 1. 长江大学地球科学学院,湖北武汉 430100
  • 2. 东方地球物理公司塔里木物探处,新疆库尔勒 841000
  • 3. 中国石油冀东油田公司勘探开发研究院,河北唐山 063004
  • 折叠

摘要

Abstract

In order to reveal the characteristics and development mechanism of Mesozoic fault system in Lunnan area,Based on the analysis method of fault structure,the types,geometric characteristics and genetic evolution of Mesozoic fault system are studied deeply in Lunnan area.The results show that the Mesozoic fracture system is dominated by tensional fault and tension-torsion fault in Lunnan area.The tensional fault system is mainly distributed in Lunxi platform area,Lunnan fault horst zone and Sangtamu fault horst zone.The fault scale of the tensional fault system is large,the profile is"eight"shaped fault combination and graben-horst structure,and the plane is NE and EW-trending banded distribution.The tension-torsion fault system is distributed in the whole area.The fault scale of the tension-torsion fault system is small,the profile is negative flower,graben and stepped combination style,and the plane is NE,and nearly SN to echelon distribution.Controlled by mid-Caledonian strike-slip faults,Mesozoic tension-torsional faults developed.Controlled by the anticlinal arching of the thrust fault in Hercynian period,Mesozoic tensional faults developed.The evolution of the fault system can be divided into three stages,namely,middle Caledonian strike-slip fault stage,Hercynian thrust fault stage and Indosinian-Yanshanian tensional fault and tension-torsion fault stage.Detailed interpretation of faults at Cambrian bottom surface to Triassic bottom surface stratigraphic interval in Lunnan area show that the No.2 tensional fault zone,No.8 and No.9 tension-torsional fault zones are the three major connect downward to the source rock of the basin.In these three areas,some faults cut upward through Cambrian bottom surface to Triassic bottom surface,which is good for hybrocarbon migration from Paleozoic to Mesozoic strata.These areas,therefore,is good for future exploration in Lunnan area.

关键词

塔里木盆地/轮南地区/中生代/断裂体系/成因机制

Key words

Tarim Basin/Lunnan area/Mesozoic/fault system/genetic mechanism

分类

天文与地球科学

引用本文复制引用

汤济广,李静,周旭,高永亮,姚嘉玮,李博文..塔里木盆地轮南地区中生界断裂体系特征及成因机制[J].长江大学学报(自然科学版),2024,21(5):1-11,11.

基金项目

国家自然科学基金项目"重力驱动深水褶皱冲断带分带差异变形机理研究:以索马里海域为例"(42002150). (42002150)

长江大学学报(自然科学版)

1673-1409

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