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川西北壤塘金成矿带中、基性岩脉及其与金成矿作用的关系
引用本文:梁斌,谢启兴,何文劲.川西北壤塘金成矿带中、基性岩脉及其与金成矿作用的关系[J].四川地质学报,2002,22(2):82-89.
作者姓名:梁斌  谢启兴  何文劲
作者单位:四川省地勘局川西北地质队,四川绵阳,621000
摘    要:在对川西北壤塘金成矿带内中-基性岩脉(闪长岩、闪长玢岩、煌斑岩)时空分布及岩相学特征调查的基础上,结合典型矿床成矿地质条件、成矿规律的研究,表明壤塘金成矿带内的中-基性岩脉与金成矿作用在时间、空间及成因上具有十分密切的关系,中-基性岩脉为金成矿作用提供了成矿物质及赋矿空间。

关 键 词:基性岩脉  中-基性岩  成矿作用  四川  金矿床  成矿地质条件
文章编号:1006-0995(2002)02-0082-04

RELATION BETWEEN INTERMEDIATE-BASIC DYKES AND GOLD ORE-FORMATION IN THE ZAMTANG GOLD MINERALIZATION ZONE, NORTHWEST SICHUAN
Liang Bin,Xie Qixing,He Wenjing.RELATION BETWEEN INTERMEDIATE-BASIC DYKES AND GOLD ORE-FORMATION IN THE ZAMTANG GOLD MINERALIZATION ZONE, NORTHWEST SICHUAN[J].Acta Geologica Sichuan,2002,22(2):82-89.
Authors:Liang Bin  Xie Qixing  He Wenjing
Abstract:A research into time-space distribution and petrographical facies of intermediate-basic (diorite, diorite porphyrite and lamprophyre) dykes in combination with geological setting and metallogenic regularities indicates that the intermediate-basic dykes are in close relationship with gold mineralization in the Zamtang gold mineralization zone, providing ore material and host space.
Keywords:intermediate-basic rock  gold mineralization  northwest Sichuan
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