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皋兰岩群时代厘定及地质意义

闫海卿 汤桦 钱壮志 徐刚

西北地质2011,Vol.44Issue(4):1-7,7.
西北地质2011,Vol.44Issue(4):1-7,7.

皋兰岩群时代厘定及地质意义

Age Determination of Gaolan Terrain and Its Geological Significance

闫海卿 1汤桦 2钱壮志 1徐刚1

作者信息

  • 1. 长安大学地球科学与资源学院,陕西西安710054
  • 2. 西安地质矿产研究所,陕西西安710054
  • 折叠

摘要

Abstract

As lack of fossil evidence and the influence of regional magma events on isotopic age determination, the geological age of the Gaolan terrain, a group of grade metamorphic rocks as the fold basement of the central Qilian block, has not been determined for a long time. During the work of the regional geological surveying of 1/250000 Lanzhou city, the authors got a large number of field geological evidence and obtained the dependable Sm-Nd isotope age of 1180. 3 Ma, which is consistent with the micro-fossils of the ancient plants from the Jixianian. The age of Gaolan terrain that is in the eastern section of central Qilian block fold basement belongs to mesoproterozoic Jixianian. It is significant to study the Central Qilian block structural properties and regional tectonic evolution.

关键词

中祁连/皋兰岩群/Sm-Nd年龄/时代厘定

Key words

Central Qilian block/ Gaolan terrain/ Sm-Nd isotope age/ age determination

分类

天文与地球科学

引用本文复制引用

闫海卿,汤桦,钱壮志,徐刚..皋兰岩群时代厘定及地质意义[J].西北地质,2011,44(4):1-7,7.

基金项目

中国地质大调查研究项目J48C004002(兰州市幅)项目(199913000218) (兰州市幅)

西北地质

OACSCDCSTPCD

1009-6248

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