新疆石油地质 ›› 1990, Vol. 11 ›› Issue (4): 276-295.

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博格达山前褶皱带的再研究

彭希龄, 胡斌, 刘楼军   

  1. 新疆石油管理局勘探开发研究院
  • 收稿日期:1990-06-26 出版日期:1990-12-01 发布日期:2020-05-19

A RESTUDY FOR PRE-BOGDA MOUNTAIN FOLDED ZONE

Peng Xiling, Hu Bin, Liu Loujun   

  1. Research Institute of Exloration and Developnent,Xinjiang Petroleum Administraticn Bureau
  • Received:1990-06-26 Online:1990-12-01 Published:2020-05-19

摘要: 博格达山前褶皱带是我国最复杂、最雄伟的山前构造单元之一。作者从彩红外航摄照片的解译入手,结合对露头的观察和近年大量勘探资料的利用,重新研究了博格达山前地区的构造,订正和描述了这个以大型带状复式背向斜和叠瓦状断裂伴生的弧状构造系统;探讨了形成机制;指出这里发育的只是大型逆掩断裂,不是推覆体;燕山期的构造特别强烈的根本原因是山前坳陷没有固化基底;博格达山前坳陷是直接继承海西地槽的晚期坳陷渐进演变而成的,故是一种新类型。

Abstract: Pre—Bogda mountain folded zone is one of the most complicate and grand tectonic unit at premountain area in China. Starting with anaiysis of the aerial colour infrared photography and combining with the survey of outcrops and use of the vast exploration data in recent years, the writers restudied the structure of pre-Bogda mountain area and correctly described this arched tectonic system which is com posed of large anticlinorium and synciinoria and imbricated faults. The writers also probed into the mechanism of formation of tectonic structure and pointed out that oniy many large reverse faults, rather than tectonic nappe, developed in here. The cardinaj cause of these particular violent structure formed in Yenshan movcmeni was the result of premountain depression without a consolidated basement. The pre—Bpgda mountain depression was formed by directly succeeded to the gradually evolution of late一Hcrcynian geosyncline, so it is a new type of pre—mountain depression.