摘要
湖北大冶鸡冠嘴矿床是鄂东南地区较典型的矽卡岩型铜金矿床，其构造位置隶属灵乡火山岩盆地东北缘，大冶复式向斜南翼，阳新中酸性岩体西北端；矿体主要赋存在岩体与大冶群（T_1dy）大理岩接触带内外及岩体内大理岩捕虏体中，明显受北北东向断裂—接触带复合构造所控制。本文主要是对该矿床的地球化学特征，主要成矿元素及其伴生元素在成矿作用中的地球化学行为进行了探讨，归纳出该矿床的地球化学找矿指标，建立地球化学找矿模式，进行深部及外围找矿预测。
:
This paper deals tentatively with geochemical characteristics of the Jigu-
anzui copper-gold deposit as well as geochemical behaviors of major ore-forming
elements and associated elements in the process of metallization. The criteria
for geochemical exploration in this ore deposit have been drawn and the
model for geochemical prospecting has been established to make ore prognosis
in depth or outskirts.
出处
《物探与化探》
CAS
CSCD
1991年第3期216-224,共9页
Geophysical and Geochemical Exploration
