|本期目录/Table of Contents|

[1]任鹏,梁婷,牛亮,等.陕西秦岭铅锌矿床的地质特征及成矿动力学过程[J].地球科学与环境学报,2013,35(01):34-47.
 REN Peng,LIANG Ting,NIU Liang,et al.Geological Characteristic and Geodynamic Process from Pb-Zn Deposit in Qinling of Shaanxi[J].Journal of Earth Sciences and Environment,2013,35(01):34-47.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第35卷
期数:
2013年第01期
页码:
34-47
栏目:
基础地质与矿产地质
出版日期:
2013-03-15

文章信息/Info

Title:
Geological Characteristic and Geodynamic Process from Pb-Zn Deposit in Qinling of Shaanxi
作者:
任鹏梁婷牛亮鲁麟张文璟杨钊王婵程玉龙
1. 长安大学西部矿产资源与地质工程教育部重点实验室;2. 长安大学地球科学与资源学院;3. 汉中市天鸿基矿业有限公司;
Author(s):
REN Peng LIANG Ting NIU Liang LU Lin ZHANG Wen-jing YANG Zhao WANG Chan CHENG Yu-long
1.Key Laboratory of Western Mineral Resources and Geological Engineering of Ministry of Education, Chang’an University,Xi’an 710054,Shaanxi,China;2.School of Earth Sciences and Resources, Chang’an University,Xi’an 710054,Shaanxi,China;3.Hanzhong Tianhongji Mining Co.,Ltd., Hanzhong 723000,Shaanxi,China
关键词:
铅锌矿地质特征物质来源成矿条件微量元素成矿动力背景秦岭陕西
Keywords:
-
分类号:
P618.4
DOI:
-
文献标志码:
-
摘要:
依据区域成矿背景、控矿构造和铅锌矿床的分布规律,将陕西秦岭铅锌矿床由北到南依次划分为凤太铅锌矿集区、山柞铅锌矿集区、镇旬铅锌矿集区以及马元铅锌矿集区。铅锌矿主要赋存在泥盆系、志留系和震旦系地层中,以热水喷流-沉积型和密西西比河谷型为主。通过对同位素地球化学、矿石矿物中微量元素地球化学特征等的总结,分析了陕西秦岭铅锌矿的成矿物质来源、成矿盆地的形成环境,进而探讨了成矿动力学过程。结果表明:陕西秦岭铅锌矿床矿石硫主要来源于海水硫酸盐,矿石铅主要来源于上地壳,成矿热液主要为大气降水;凤太铅锌矿集区、山柞铅锌矿集区、镇旬铅锌矿集区大规模的成矿作用受控于晚古生代扬子板块和秦岭微板块分别沿勉略带和商丹带俯...
Abstract:
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参考文献/References:

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备注/Memo

备注/Memo:
中国地质调查局地质大调查项目(1212011120354)
更新日期/Last Update: 2013-01-20