| 注册
首页|期刊导航|地质论评|班公湖—怒江结合带西段沙木罗组底砾岩的新发现及地质意义

班公湖—怒江结合带西段沙木罗组底砾岩的新发现及地质意义

邓金火 钟俊靖 袁振国 余江 杜昌法 唐宗源 孙社良 吕鑫 钟文 万川

地质论评2017,Vol.63Issue(2):302-310,9.
地质论评2017,Vol.63Issue(2):302-310,9.DOI:10.16509/j.georeview.2017.02.004

班公湖—怒江结合带西段沙木罗组底砾岩的新发现及地质意义

New Discovery of the Basal Conglomerate in the Upper Jurassic—Lower Cretaceous Shamuluo Formation in Western Part of Bangong Lake—Nujiang River Suture Zone and Its Geological Significance

邓金火 1钟俊靖 1袁振国 1余江 1杜昌法 1唐宗源 2孙社良 1吕鑫 1钟文 1万川1

作者信息

  • 1. 江西省地质调查研究院,南昌,330030
  • 2. 吉林大学地球科学学院,长春,130061
  • 折叠

摘要

Abstract

Late Jurassic—Early Cretaceous Shamuluo Formation outcropped along the middle—western segment of the Bangongco—Nujiang Belt.Upper Jurassic shore—shallow marine deposits are formed in relatively stable environments,Shamuluo Formation,was named after Shamuluo area of the southern Yanhu district of Geji country.The Structural Belt has been divided into Mugagangri Group and Shamuluo Formation by many geologists based on in different regions,but the stratigraphic sequence division of the two strata has always been characterized by lithologic assemblage difference or granule change.However,they haven't gotten the solid evidence of angular unconformity.At the bottom of the Shamuluo Formation in the Gengze area,the author discovered for the first time the top clayey weathering crust of the basal conglomerate and the underlying Mugagangri Group,which proved that the unconformitty of the two formations is credible.And then to determine the angle unconformity contact relationship between the Shamuluo Formation and the underlying Mugagangri Group.The discovery of the basal conglomerate is of great geological significance in studying the tectonic evolution of the Neo-Tethys ocean,the paleogeographic environment,the lower age limit of the Shamuluo Formation stratigraphy and the sedimentary facies.

关键词

班公湖—怒江结合带/沙木罗组/底砾岩/角度不整合接触

Key words

Bangong Co—Nujiang Juctional Zone/Shamuluo Formation/Basal Conglomerate/Angular Unconformity

引用本文复制引用

邓金火,钟俊靖,袁振国,余江,杜昌法,唐宗源,孙社良,吕鑫,钟文,万川..班公湖—怒江结合带西段沙木罗组底砾岩的新发现及地质意义[J].地质论评,2017,63(2):302-310,9.

基金项目

本文为中国地质调查“西藏康托地区矿产远景调查”项目(编号:12120113037600)资助的成果.This research was financially supported by the project from China Geological Survey Grant (No:12120113037600) (编号:12120113037600)

地质论评

OA北大核心CSCDCSTPCD

0371-5736

访问量4
|
下载量0
段落导航相关论文