|本期目录/Table of Contents|

[1]吴夏涛,周家喜*,张 浩,等.川滇黔接壤地区铅锌矿床成矿物质来源:方铅矿原位Pb同位素制约[J].地球科学与环境学报,2023,45(02):266-278.[doi:10.19814/j.jese.2022.11027]
 WU Xia-tao,ZHOU Jia-xi*,ZHANG Hao,et al.Source of Ore-forming Materials for the Carbonate-hosted Pb-Zn Deposits in Sichuan-Yunnan-Guizhou Adjacent Area, SW China: Constraints of Galena In-situ Pb Isotopes[J].Journal of Earth Sciences and Environment,2023,45(02):266-278.[doi:10.19814/j.jese.2022.11027]
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川滇黔接壤地区铅锌矿床成矿物质来源:方铅矿原位Pb同位素制约(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第45卷
期数:
2023年第02期
页码:
266-278
栏目:
基础地质与矿床地质
出版日期:
2023-03-15

文章信息/Info

Title:
Source of Ore-forming Materials for the Carbonate-hosted Pb-Zn Deposits in Sichuan-Yunnan-Guizhou Adjacent Area, SW China: Constraints of Galena In-situ Pb Isotopes
文章编号:
1672-6561(2023)02-0266-13
作者:
吴夏涛123周家喜12*张 浩12杨昌华4罗 开12姜永果4张亚辉12
(1. 云南大学 地球科学学院,云南 昆明 650500; 2. 云南大学 云南省高校关键矿产成矿学重点实验室,云南 昆明 650500; 3. 云南铜业矿产资源勘查开发有限公司,云南 昆明 650051; 4. 云南省有色地质局地质地球物理化学勘查院,云南 昆明 650216)
Author(s):
WU Xia-tao123 ZHOU Jia-xi12* ZHANG Hao12 YANG Chang-hua4 LUO Kai12 JIANG Yong-guo4 ZHANG Ya-hui12
(1. School of Earth Sciences, Yunnan University, Kunming 650500, Yunnan, China; 2. Key Laboratory of Critical Minerals Metallogeny in Universities of Yunnan Province, Yunnan University, Kunming 650500, Yunnan, China; 3. Yunnan Copper Mineral Resources Exploration and Development Co. LTD, Kunming 650051, Yunnan, China; 4. Institute of Geology, Geophysics and Geochemistry Exploration, Yunnan Nonferrous Geological Bureau, Kunming 650216, Yunnan, China)
关键词:
铅锌矿床 方铅矿 Pb同位素 成矿物质来源 成矿流体 太古代—古元古代 结晶基底 川滇黔接壤地区
Keywords:
Pb-Zn deposit galena Pb isotope source of ore-forming material ore-forming fluid Archean-Paleoproterozoic crystalline basement Sichuan-Yunnan-Guizhou adjacent area
分类号:
P597+.1; P612
DOI:
10.19814/j.jese.2022.11027
文献标志码:
A
摘要:
位于扬子板块西南缘的川滇黔铅锌矿集区,是我国以碳酸盐岩为容矿岩石的铅锌矿产最为集中发育的区域,在我国铅锌成矿区/带中占有重要地位。尽管以往研究取得了丰硕的理论认识和找矿成果,但是对研究区铅锌矿床的成矿物质来源一直存有争议。以9个赋存于震旦系(乌斯河、赤普、银厂沟和茂租矿床)、泥盆系(火德红、毛坪和猫榨厂矿床)和石炭系(毛坪、会泽、亮岩和猫榨厂矿床)中的铅锌矿床为例,进行了较为系统的方铅矿原位Pb同位素地球化学综合研究。结果表明:①乌斯河、赤普、银厂沟、茂租、火德红、毛坪、猫榨厂、会泽、亮岩矿床原位Pb同位素组成的线性关系明显,其Pb-Pb等时线年龄约为2.5 Ga((2 574±30)Ma),暗示这些矿床的成矿物质来源相同,且太古代—古元古代结晶基底岩石是最可能的主要金属源区; ②在赋矿地层时代上,Pb同位素组成由老(震旦系)至新(石炭系)逐渐增加; 在赋矿层位空间上,Pb同位素组成由北(西)部的乌斯河、赤普矿床向南(东)部的猫榨厂、亮岩矿床逐渐增加; 这些特征暗示其是同一成矿流体不同演化阶段的产物,且在区域尺度上来源或流经结晶基底岩石的成矿流体由深部向浅部、由北(西)向南(东)方向运移演化。
Abstract:
The Sichuan-Yunnan-Guizhou Pb-Zn metallogenic province, located in the southwestern margin of the Yangtze Block, is the most intensively developed region of carbonate-hosted Pb-Zn deposits in China. Both the number of Pb-Zn deposits/spots(more than 500)and the amount of Pb and Zn metal reserves(more than 2 000×104 t)play an important role in the Pb-Zn metallogenic regions/belts of China. Although the previous research has made fruitful theoretical understanding and prospecting achievements, there has been a dispute on the source of ore-forming materials of the Pb-Zn deposits in the study area. A systematic In-situ Pb isotope analysis of galena from nine Pb-Zn deposits hosted in the Sinian(Wusihe, Chipu, Yinchanggou and Maozu deposits), Devonian(Huodehong, Maoping and Maozachang deposits)and Carboniferous(Maoping, Huize, Liangyan and Maozachang deposits)carbonate rocks was carried out. The results show that ① the In-situ Pb isotopes of galena in all deposits have an obvious linear relationship, and their Pb-Pb isochron age is about 2.5 Ga((2 574±30)Ma); it is suggested that the sources of ore-forming metals for these deposits are the same, and the Archean-Paleoproterozoic crystalline basement rocks are the most likely major metal source; ② in the age of ore-bearing strata, the Pb isotopes gradually increase from the old(Sinian)to the new(Carboniferous); in the space of ore-bearing horizon, the Pb isotopes gradually increase from Wusihe, Chipu deposits in N(W)to Maozachang, Liangyan deposits in S(E); it is indicated that they are the evolvement products of the same ore-forming fluids in different stages, and the crystalline basement-derived and/or flowed ore-forming fluids evolve and migrate from deep to shallow, and from N(W)to S(E)on a regional scale.

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备注/Memo

备注/Memo:
收稿日期:2022-11-09; 修回日期:2023-01-15
基金项目:国家自然科学基金项目(41872095,42172082,U1812402); 云南省科技厅重点项目(2019FY003029); 云南大学科研启动项目(YJRC4201804); 云南大学关键金属成矿与找矿预测创新团队项目(2021-3)
作者简介:吴夏涛(1984-),男,湖北武穴人,云南铜业矿产资源勘查开发有限公司高级工程师,E-mail:txwxt@chncopper.com。
*通讯作者:周家喜(1982-),男,安徽霍邱人,研究员,博士研究生导师,理学博士,E-mail:zhoujiaxi@ynu.edu.cn。
更新日期/Last Update: 2023-05-20