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甘肃东海金矿地质特征及成因探讨
引用本文:刘堆富,赵立春.甘肃东海金矿地质特征及成因探讨[J].地质找矿论丛,2002,17(2):97-102.
作者姓名:刘堆富  赵立春
作者单位:1. 中国地质大学,武汉,湖北,武汉,430074;甘肃有色地质勘查局四队,甘肃,张掖,734012
2. 甘肃省安西县矿管局,甘肃,安西,735000
摘    要:文章阐述了东海金矿地层,构造,侵入岩,矿体特征,围岩蚀变及矿床硫,铅同位素特征,指出了矿体受控于构造和华力西中晚期酸性侵入岩,总结了矿化富集规律,认为该矿床具有多因复成矿床之“五多”之特点。

关 键 词:地质特征  矿床成因  东海金矿  甘肃
文章编号:1001-1412(2002)02-0097-06
收稿时间:2001/11/29 0:00:00
修稿时间:2002/4/3 0:00:00

GEOLOGICAL FEATURES AND ORIGIN OF DONGHAI GOLD DEPOSIT IN GANSU
LIU Duifu and ZHAO Lichun.GEOLOGICAL FEATURES AND ORIGIN OF DONGHAI GOLD DEPOSIT IN GANSU[J].Contributions to Geology and Mineral Resources Research,2002,17(2):97-102.
Authors:LIU Duifu and ZHAO Lichun
Institution:LIU Dui-fu 1,2,ZHAO Li-chun 3
Abstract:The article elaborated scientifically the features of stratigraphy, structure, volcanic rocks, alteration of wall rocks and ore bodies. Ore bodies are controlled by structures and Middle-Late Variscian intrussive rock, volcanic rocks, and then is summarized the regular patterns of mineral concentration. At last the author made a discussion about the origin of Donghai gold deposit in Gansu,i.e. polygenetic compound ore deposit.
Keywords:geological features  ore genesis  Donghai gold deposit  Gansu
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