抱板金矿带金矿床地质特征和成矿规律  

STUDY ON ORE DEPOSIT GEOLOGICAL FEATURE AND METALLOGENIC REGULARITY OF BAOBAN GOLD ORE BELT IN HAINAN PROVINCE

作　　者：秦联 俞受鋆[2] 

机构地区：[1]武警黄金一总队,哈尔滨150086 [2]中山大学地质系

出　　处：《矿产与地质》1993年第1期8-13,共6页Mineral Resources and Geology

基　　金：国家自然科学基金资助项目

摘　　要：矿带中的金矿床以破碎带蚀变岩型金矿为主,金矿化与蚀变作用、燕山期岩脉、NE向戈枕断裂及环形构造关系密切.矿带具有多缀控矿构造,矿床分布具有等距性.The gold deposits in fractured zone-alteration rock is the main type in Baoban Gold Belt. The minerogene-sis is mainly related to the alteration, Yenshanian dikes,NE trending Gezhen fault belt and circular structure. There are various scales of ore-controlling fractures in the gold belt and the gold deposits are distributed with e-qui-distance.

关 键 词：金矿带 金矿床 地质特征 成矿规律 

分 类 号：P618.510.2[天文地球—矿床学]