文章摘要
伊有昌,董想平,杜占美,袁克全,曹守林.祁连山黑河上游地区沉积变质型铁矿成矿地质条件分析[J].矿产勘查,2015,6(4):397-404
祁连山黑河上游地区沉积变质型铁矿成矿地质条件分析
Analysis of metallogenic conditions of metamorphic sedimentary iron ore deposit in the upper stream of the Black River along Qilian mountain range
  
DOI:
中文关键词: 地质特征  铁矿  热水沉积变质型  黑河
英文关键词: geological characteristics, iron deposit, metamorphic sedimentary type, the Black River area
基金项目:青海省矿产资源调查评价项目(编号:1212011121214)资助。
作者单位
伊有昌 青海省有色地质矿产勘查局七队,西宁 810007 
董想平 青海省有色地质矿产勘查局七队,西宁 810007 
杜占美 青海省有色地质矿产勘查局七队,西宁 810007 
袁克全 青海省有色地质矿产勘查局七队,西宁 810007 
曹守林 青海省有色地质矿产勘查局七队,西宁 810007 
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中文摘要:
      文章初步总结了黑河上游地区铁矿分布特征,按其地理分布、成矿时代、含矿建造及成矿地质特征,可划分为走廊南山铁矿带(北带)和托勒山铁矿带(南带)两个成矿带,含矿岩系为泥钙质硅质板岩,层位延伸较稳定,具有一定的层控性,矿石具明显层纹状、条带状构造,其铁矿床成因类型为热水沉积变质型。通过对矿床成因和成矿地质条件分析研究,总结出了该地区成矿找矿模式,提出了进一步的找矿方向。
英文摘要:
      The distribution characteristics of iron deposits in the upper stream of the Black River, Qilian mountain range are preliminarily summarized in the paper. The iron deposits mainly distribute along two sub-belts in the region. The host strata mainly is mud calcareous siliceous slate which extends stable in layer form, therefore the deposit has the characteristics of strata-bound type. The ore texture has apparent laminar and banded structures. The iron deposit is classified into the metamorphic hydrothermal sedimentary deposit. Based on the study of deposit genesis and ore-forming geological conditions, the metallogenic and prospecting models in this area were set up, and prospecting targets were outlined for further exploration in this region. 
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