Geological Characteristics and and prospect of Changchungou-Dagaitan lead-zinc deposit in Huade county,Inner Mongolia
Received:July 15, 2018  Revised:July 20, 2018
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KeyWord:lead-zinc deposits,geological characters,prospecting indicators,Huade county,Changchungou-Dagaitan.
              
AuthorInstitution
liujunjie 内蒙古自治区地质勘查基金管理中心
赵九峰 内蒙古国土资源勘查开发院
秦增刚 内蒙古自治区地质勘查基金管理中心
崔来旺 内蒙古自治区地质勘查基金管理中心
孙连云 内蒙古自治区地质调查院
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Abstract:
      Abstrect:The Changchungou-Dagaitan lead-zinc deposits is a newly discovered polymetallic deposit,which the formation of such ore deposits is closely in related to Mesozoic tectonic magmatic activities and mineralization. The type of mineralization is hydrothermal filling polymetallic deposit. The ore layer is veinlike、stratiform-like structures。it is strictly controlled by the rock mass and specific stratigraphy horizon,distributed in NW-trending Fault Zone。The geochemical anomalies are closely related to the distribution of mineralization alteration zone. The geochemical anomaly and wall-rock alteration are important ore prospecting symbols. By studying the geological background and ore-forming geological conditions in the region, The main ore control factors、orebody characteristics and prospecting criteria are summarized and the prospecting prospects are discussed in this paper, with further prospecting direction is put forward. Key words:lead-zinc deposits,geological characters,prospecting indicators,Huade county,Changchungou-Dagaitan.
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