[an error occurred while processing this directive] 世界地质 2020, 39(3) 544-556 DOI:   10.3969/j.issn.1004-5589.2020.03.004  ISSN: 1004-5589 CN: 22-1111/P

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本文关键词相关文章
归来庄金矿
矿体特征
矿床成因
成矿模型
本文作者相关文章
索晓晶
刘顺好
李胜荣
朱金
马媛
周慧君
PubMed
Article by Suo X
Article by Liu S
Article by Li S
Article by Zhu J
Article by Ma Y
Article by Zhou H
山东归来庄金矿床地质特征及成矿模型
索晓晶1,2, 刘顺好3, 李胜荣1, 朱金1, 马媛1, 周慧君1
1. 中国地质大学地质过程与矿产资源实验室, 北京 100083;
2. 武警黄金第二支队, 呼和浩特 010011;
3. 山东黄金归来庄矿业有限公司, 山东临沂 273306
摘要: 为查明山东归来庄金矿的成因信息和成矿过程,笔者通过系统梳理成矿地质背景和矿床地质特征,并运用黄铁矿Rb-Sr、碳氧稳定同位素和流体包裹体等方法,查明归来庄金矿是中低温成矿流体经过多期次、多阶段演化,形成于中侏罗世晚期的矿床。在此基础上结合前人研究成果,建立了成矿模型。
关键词 归来庄金矿   矿体特征   矿床成因   成矿模型  
Geologic feature and metallogenic model of Guilaizhuang gold deposit, Shandong
SUO Xiao-jing1,2, LIU Shun-hao3, LI Sheng-rong1, ZHU Jin1, MA Yuan1, ZHOU Hui-jun1
1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China;
2. No.2 Gold Geological Party of CAPF, Hohhot 010011, China;
3. Shandong Gold Guilaizhuan Deposit Co. Ltd., Linyi 273306, Shangdong, China
Abstract: To understand the genesis information and ore-forming process, the pyrite Rb-Sr, stable C-O isotope and fluid inclusion analyses are used in combination with the systematic study of metallogenic geological background and geological characteristics of gold deposit in Guilaizhuang gold mine, Shandong Province. The results show that Guilaizhuang gold deposit is formed by multiple-stage evolution of medium-low temperature hydrothermal fluid in the late Middle Jurassic. The metallogenic model is then established based on this study and previous research results.
Keywords: Guilaizhuang gold deposit   orebody characteristics   genesis   metallogenic model  
收稿日期 2019-08-05 修回日期 2020-04-25 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2020.03.004
基金项目:

国家重点研发计划课题(2016YFC0600106)

通讯作者: 李胜荣(1956-),男,教授,主要从事成因矿物学与找矿矿物学研究。E-mail:1617948383@qq.com
作者简介:
作者Email: 1617948383@qq.com

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