贵州海马谷地区金矿矿床特征及成矿模式  

Characteristics and Metallogenic Mode of Gold Deposit in Haimagu Area of Guizhou

作　　者：曾昭光[1] 杨恩林[1] 季国松[1] 向通[1] 

机构地区：[1]贵州省地矿局117地质大队,贵州贵阳550018

出　　处：《贵州地质》2014年第4期261-266,共6页Guizhou Geology

摘　　要：本文对海马谷地区金矿进行调查,在贵州安龙海马谷发现北东向陡倾角断层控制金矿体,其围岩为二叠系茅口组生物灰岩,矿石为硅化灰岩角砾岩。根据本次调查及收集已有勘查研究成果,建立了该区的成矿模式,认为该区北东向陡倾角断层是下一步该区重要的找矿目标。In this paper, it investigates the gold deposit in Haimagu area, NE high dip angle fauh-controlled gold deposit is found in Haimagu of Anlong, its wall-rock is biolithite limestone of Maokou formation in Pernian, the ore is silicified limestone breccia. According to this investigation and former information, the metallogenic mode is built up, it＇ s thought the NE high dip angle fault in this area is an important target in the next step.

关 键 词：贵州 海马谷 陡倾角断层 金矿特征 找矿远景 

分 类 号：P618.51[天文地球—矿床学]