|本期目录/Table of Contents|

[1]卢树东,汪石林,高文亮,等.江西德安黄金洼锡矿地质特征及控矿因素[J].地球科学与环境学报,2006,28(01):17-23.
 LU Shu-dong,WANG Shi-lin,GAO Wen-liang,et al.Geological Feature and Ore-control Factors of Huangjinwa Sn Despoit,De’ an County in Jiangxi Province[J].Journal of Earth Sciences and Environment,2006,28(01):17-23.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第28卷
期数:
2006年第01期
页码:
17-23
栏目:
出版日期:
2006-03-15

文章信息/Info

Title:
Geological Feature and Ore-control Factors of Huangjinwa Sn Despoit,De’ an County in Jiangxi Province
作者:
卢树东1汪石林2高文亮2肖锷2许建华2
1.中国地质大学岩石圈构造深部过程及探测技术教育部重点实验室,北京100083; 2.江西省地质矿产勘查局916地质大队,江西九江332100
Author(s):
LU Shu-dong1WANG Shi-lin2GAO Wen-liang 2XIAO E2XU Jian-hua2
1. Key Laboratory for Lithospheric Structure and Exploration Techtonics and Lithoprobing Technology o f Ministry of Education, China University of Geosciences, Beijing 100083, China; 2. No.916 Geological Party, Jiangxi Bureau of Geology and Mineral Resources, Jiujiang 332100, Jiangxi, China
关键词:
锡矿地质特征控矿因素黄金洼江西省
Keywords:
Zn deposit geological feature ore-control factors Huangjinwa Jiangxi Province
分类号:
P618.440.1
DOI:
-
文献标志码:
A
摘要:
介绍了黄金洼锡矿矿体特征,分析了控矿因素,讨论了成矿作用,指出该矿床的形成是多种地质因素综 合作用的结果。地处九瑞地区有利多金属成矿带,燕山晚期中酸性花岗岩体的产生是成矿作用发生的起始条 件,区内丰富的多级断裂构造体系为岩浆、成矿流体运移和最终就位提供了运、储、移的重要空间,尤其是断层 F1和F4之间所形成的次一级密集北西—北西西向裂隙带成为成矿流体汇聚的重要场所,成为主要的矿产聚集 地。矿床的形成是多阶段成矿作用的产物,矿物质经历了富集、活化、再次富集、定位成矿的复杂过程。
Abstract:
This paper introduces in detail the orebody feature, ore-controlling factors and metallogenesis of the Huangjinwa Zn deposit. Many evidences show that the forming of deposit is the result of multifold factor-control- ling. First, the medium-acidic granite body formed in the late Yanshanian period created the precondition of ore- forming. Second, abundance multilevel tectonic system provided some important spaces of carrying, moving and storing for magma and ore-forming liquid. Especially the secondary intensive fissures with NW-NWW strike be- tween F1and F4faults became the main room of ore-forming fluid gathering finally. The whole deposit-forming experienced a multistage metallogenesis process. Mineral substances suffered a complex history of enrichment, activation, ore-enrichment and location.

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备注/Memo

备注/Memo:
[收稿日期]2005-03-21
[基金项目]中国地质调查局地质调查项目(K132)
[作者简介]卢树东(1973-),男,江西九江人,工程师,从事矿床学、矿物学和岩石学研究。
更新日期/Last Update: 2006-03-20