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新疆尼勒克县乔尔玛铁矿床地质特征及成因初探

韩继全 许新芳 赵洋

地质调查与研究2016,Vol.39Issue(3):204-209,6.
地质调查与研究2016,Vol.39Issue(3):204-209,6.

新疆尼勒克县乔尔玛铁矿床地质特征及成因初探

Geological Characteristics of the Qiaoerma iron deposit in Nileke, Xinjiang province

韩继全 1许新芳 1赵洋1

作者信息

  • 1. 新疆地质矿产勘查开发局第一区域地质调查大队,乌鲁木齐 830013
  • 折叠

摘要

Abstract

The Qiaoerma ore deposits lies in the northeastern margin of the Yili Block, produced in Lower Carboniferous Dahalajunshan formation volcanic rocks. Mineralization rock is acidic tuff welded tuff, andesitic lithic tuff and andesitic volcanic breccia. Through regional geology, deposit geological characteristics, comparative study of the adjacent iron ore deposit geological characteristics and features within the same metallogenic belt,it is suggested that Qiaoerma iron ore genesis type belongs to volcanic hydrothermal iron deposit with a great prospect.

关键词

乔尔玛/地质特征/找矿标志/矿床成因

Key words

Qiaoerma iron deposit/geological characteristic/prospecting indication/deposit origin

分类

地质学

引用本文复制引用

韩继全,许新芳,赵洋..新疆尼勒克县乔尔玛铁矿床地质特征及成因初探[J].地质调查与研究,2016,39(3):204-209,6.

基金项目

新疆西天山那拉提山东段金铁多金属矿调查评价项目 ()

地质调查与研究

1672-4135

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