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甘肃肃北县鹰嘴山金矿矿质来源分析及成矿模式探讨
引用本文:沈清杰,许文进.甘肃肃北县鹰嘴山金矿矿质来源分析及成矿模式探讨[J].甘肃地质学报,2011(1):43-51.
作者姓名:沈清杰  许文进
作者单位:甘肃省地矿局第四地勘院;
摘    要:通过对鹰嘴山金矿容矿围岩的研究及加里东期超基性岩含金性的评价,认为鹰嘴山金矿的金主要来自超基性岩,而且超基性岩浆的侵入为黒茨沟组火山岩中微量金的加剧活化提供了热力条件。同时研究了断裂控矿性质、矿床地球化学特征认为,鹰嘴山金矿是一个与超基性有关的中低温热液型金矿床,提出了成矿模式。

关 键 词:鹰嘴山金矿  矿质来源  同位素地球化学  流体包裹体  成矿时代  成矿模式

DISCUSSION ON METALLOGENETIC MATERIAL SOURCES AND MODEL OF YINGZUISHAN GOLD DEPOSIT
SHEN Qing-jie and XU Wen-jin.DISCUSSION ON METALLOGENETIC MATERIAL SOURCES AND MODEL OF YINGZUISHAN GOLD DEPOSIT[J].Acta Geologica Gansu,2011(1):43-51.
Authors:SHEN Qing-jie and XU Wen-jin
Institution:SHEN Qing-jie,XU Wen-jin(No.4 Geology and Mineral Exploration Team,Gansu Provincial Bureau of Geology and Mineral Exploration and Development,Jiuquan 735000,China)
Abstract:The authors support that the gold of Yingzuishan gold deposit was mainly originated from ultra-mafic rocks,and the invasion of the ultramafic rocks provided the heat condition for the action of trace gold in igneous rocks of Heicigou Formation.The studies of ore-control structures and geochemical features show that Yingzushan gold deposit is a meso-eqithermal deposit.
Keywords:Yingzuishan gold deposit  ore source  isotopic geochemistry  fluid inclusions  metallogenetic epoch  metallogenetic model  
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