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“三江”地区哀牢山带两类硅质岩 特征及大地构造意义

沈上越 魏启荣 程惠兰 莫宣学

岩石矿物学杂志2001,Vol.20Issue(1):42-46,5.
岩石矿物学杂志2001,Vol.20Issue(1):42-46,5.

“三江”地区哀牢山带两类硅质岩 特征及大地构造意义

Characteristics and Geotectonic Implications of Two Sorts of Silicalites in Ailao Mountain Belt, “Three_River” Area

沈上越 1魏启荣 1程惠兰 1莫宣学1

作者信息

  • 1. 中国地质大学材料与化学学院,
  • 折叠

摘要

Abstract

Late Devonian (D3) silicate and Early Carboniferous (C1) silicatein Ailao Mountain belt, “Three_River” area, are quite different from each other in mode of occurence, Radiolaria association, Si isotope and REE character. The former was formed in a deep_sea environment, i.e., in an intracontinental rift, whereas the latter is a component unit of Ailao Mountain ophiolite suite formed in a bathyal environment, indicating that Ailao Mountain was a small oceanic basin at that time.

关键词

“三江”地区/哀牢山带/硅质岩/放射虫/硅同位素/稀土元素

分类

天文与地球科学

引用本文复制引用

沈上越,魏启荣,程惠兰,莫宣学..“三江”地区哀牢山带两类硅质岩 特征及大地构造意义[J].岩石矿物学杂志,2001,20(1):42-46,5.

基金项目

本文得到国家自然科学基金( ()

岩石矿物学杂志

OA北大核心CSCD

1000-6524

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