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黔中-渝南铝土矿含矿岩系时代探讨

刘平 廖友常

中国地质2012,Vol.39Issue(3):661-682,22.
中国地质2012,Vol.39Issue(3):661-682,22.

黔中-渝南铝土矿含矿岩系时代探讨

A tentative discussion on the age of bauxite-bearing rock series in Central Guizhou-Southern Chongqing area

刘平 1廖友常1

作者信息

  • 1. 贵州省地质矿产勘查开发局106地质大队,贵州遵义563000
  • 折叠

摘要

Abstract

Bauxite has been discovered since 1940's in Guizhou, and the emphasis of the study have been placed on the generation age of bauxite -bearing rock series. In this paper, a lithographic description of central Guizhou -northern Guizhou -southern Chongqing area was given on the basis of nine standard sections of bauxite-bearing rock series, and a detailed statistic analysis was made for sporo-pollen genera and species widely distributed in Carboniferous Jiujialu Formation and Dazhuyuan Formation and middle Permian Liangshan Formation. Based on data available and related geological characteristics, the authors hold that the age of Jiujialu Formation in Qingzhen and Xiuwen of central Guizhou to Zunyi area and their vicinities belongs to early -middle Datang period of early Carboniferous, and Dazhuyuan Formation in northern Guizhou -southern Chongqing area should be early Maping period of late Carboniferous.

关键词

铝土矿含矿岩系时代/九架炉组/大竹园组/石炭系/黔中—渝南

Key words

age of bauxite-bearing rock series/ Jiujialu Formation/ Dazhuyuan Formation/ Carboniferous/ central Guizhou-southern Chongqin area

分类

天文与地球科学

引用本文复制引用

刘平,廖友常..黔中-渝南铝土矿含矿岩系时代探讨[J].中国地质,2012,39(3):661-682,22.

中国地质

OA北大核心CSCDCSTPCD

1000-3657

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