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内蒙古大梁道班地区本巴图组地层时代的确定及其地质意义

姜振宁 孟都

化工矿产地质2016,Vol.38Issue(1):33-37,5.
化工矿产地质2016,Vol.38Issue(1):33-37,5.

内蒙古大梁道班地区本巴图组地层时代的确定及其地质意义

AGE DETERMINATION OF BENBATU FORMATION AND THE GEOLOGICAL SIGNIFICANCE OF DALIANGDAOBAN, INNER MONGIOLIA

姜振宁 1孟都1

作者信息

  • 1. 中化地质矿山总局地质研究院,河北涿洲,072754
  • 折叠

摘要

Abstract

The Benbatu Formation take large area of Daliangdaoban in Inner Mongolia. They deform intensively and metamorphose lightly caused by magma movement and tectogenesis, therefore, there are complex rock combination types and blurry stratum sequence with jumbled structure which are different with the regional Bumbat Formation. We found the stratum were developed in late permian system according to the reseach on the rock combination and isotopic age testing as well as the analysis of fossil organism. They also found that the Siberia plate joint North China plate at late Permian period and early Triassic System.

关键词

本巴图组/地层时代/地质意义/大梁道班/内蒙古

Key words

Bumbat formation/stratum era/geological signification/Daliangdaoban,Inner Mongolia

分类

天文与地球科学

引用本文复制引用

姜振宁,孟都..内蒙古大梁道班地区本巴图组地层时代的确定及其地质意义[J].化工矿产地质,2016,38(1):33-37,5.

化工矿产地质

1006-5296

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