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灵山沟金矿围岩蚀变形成机制酸碱演化特征及对成矿作用的意义
引用本文:敬成贵,魏震环.灵山沟金矿围岩蚀变形成机制酸碱演化特征及对成矿作用的意义[J].矿产与地质,1992,6(5):369-374.
作者姓名:敬成贵  魏震环
作者单位:天津地质研究院 300061 (敬成贵),天津地质研究院 300061(魏震环)
摘    要:通过对灵山沟金矿围岩蚀变带特征的研究,阐明了灵山沟金矿围岩蚀变以碱交代为主,成矿热液为壳源深熔花岗岩浆演化期后热液,并指出围岩蚀变的发育程度与金矿化有密切的关系。

关 键 词:围岩蚀变  金矿床  成矿作用  形成

WALL ROCK ALTERATION MECHANISM AND ALKALITY - ACIDITY EVOLUTION FEATURES AND THEIR SIGNIFICANCE TO METTALLOGENESIS OF LINGSHANGOU GOLD DEPOSIT,EASTERN SHANDONG PROVINCE
Jing Chenggui,Wei Zhenhuan.WALL ROCK ALTERATION MECHANISM AND ALKALITY - ACIDITY EVOLUTION FEATURES AND THEIR SIGNIFICANCE TO METTALLOGENESIS OF LINGSHANGOU GOLD DEPOSIT,EASTERN SHANDONG PROVINCE[J].Mineral Resources and Geology,1992,6(5):369-374.
Authors:Jing Chenggui  Wei Zhenhuan
Abstract:On the basis of the study of the features of wall rock alteration zoning in Lingshangou gold deposit. It is indicated that the alkali-metasomatism played the leading role in wall rock alteration and the ore-forming fluid was from post magmatic hydrothermal soluion crust-derived anatectic granite .and the developing degree of wall rock alteration is closely related to gold mineralization.
Keywords:Nothwestern Shandong  Wall rock alteration  alkali metasomatism  Gold ore deposit  
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