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四川省黑水县四美沟锰矿床地质特征及成因
引用本文:刘波,林雄,张姚,邓元兵.四川省黑水县四美沟锰矿床地质特征及成因[J].四川地质学报,2014(2):195-199,207.
作者姓名:刘波  林雄  张姚  邓元兵
作者单位:[1]成都理工大学,成都610059 [2]四川省冶金地质勘查局水文工程大队,四川郫县611730
摘    要:四美沟锰矿处于瓦钵梁子—四美沟复式背斜西段北翼,次级北西向指状罗白背斜核部中段的两翼。矿区包括多瓦矿点和各百窝矿点。该矿床的含矿层位为菠茨沟组中段,已在多瓦矿点中发现锰矿体10条,其中工业矿体3条;在各百窝矿点中锰矿体4条,其中工业矿体1条。经对该矿床成因及成矿演化的分析认为,该矿床属沉积变质型矿床,有六条找矿标志。

关 键 词:锰矿  地质特征  矿床成因  四美沟

Geological Features and Genesis for the Simeigou Mn Deposit in Heishui,Sichuan
LIU Bo,LIN Xiong,ZHANG Yao,DENG Yuan-bing.Geological Features and Genesis for the Simeigou Mn Deposit in Heishui,Sichuan[J].Acta Geologica Sichuan,2014(2):195-199,207.
Authors:LIU Bo  LIN Xiong  ZHANG Yao  DENG Yuan-bing
Institution:1.Chengdu University of Technology, Chengdu 610059; 2.Hydrogeological and Engineering Geological Party, Sichuan Bureau of Metallurgical Geological Exploration, Chengdu 611730)
Abstract:The Simeigou Mn deposit in Heishui, Sichuan lies in the Waboliangzi-Simeigou anticlinorium and is confined to the Middle Member of the Bocigou Formation. This paper deals with geological features and sedimentary metamorphic genesis of the deposit.
Keywords:Mn deposit  geological feature  ore genesis  Simeigou
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