藏南扎西康铅锌多金属矿床成因——硫化物原位硫同位素证据

doi:10.13278/j.cnki.jjuese.20190287

吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (5): 1289-1303.doi: 10.13278/j.cnki.jjuese.20190287

• 整装勘查区矿床成因与成矿作用研究专辑 • 上一篇下一篇

藏南扎西康铅锌多金属矿床成因——硫化物原位硫同位素证据

李洪梁¹, 李光明^2,3, 丁俊^2,3, 张志², 卿成实², 付建刚², 凌晨^2,3, 刘宇奇^2,3

1. 中国地质科学院探矿工艺研究所, 成都 611734;
2. 中国地质调查局成都地质调查中心, 成都 610081;
3. 成都理工大学地球科学学院, 成都 610059

收稿日期:2019-11-20 出版日期:2020-09-26 发布日期:2020-09-29
通讯作者: 李光明(1965-),男,研究员,博士,主要从事青藏高原区域与矿产地质方面的研究,E-mail:li-guangming@163.com E-mail:li-guangming@163.com
作者简介:李洪梁(1990-),男,博士研究生,主要从事青藏高原地质矿产勘查评价方面的研究,E-mail:siliang2222@126.com
基金资助:
国家自然科学基金项目（41702080，91955208，41602214）；中国地质调查局项目（DD20190644，DD20190147）；国家科学技术部科技支撑计划重点项目（2016YFC060308，2018YFC0604103）

Genesis of Zhaxikang Pb-Zn Polymetallic Deposit in Southern Tibet: Evidence from in Situ S Isotopes of Sulfides

Li Hongliang¹, Li Guangming^2,3, Ding Jun^2,3, Zhang Zhi², Qing Chengshi², Fu Jiangang², Ling Chen^2,3, Liu Yuqi^2,3

1. Institute of Exploration Technology, Chinese Academy of Geological Sciences, Chengdu 611734, China;
2. Chengdu Center, China Geological Survey, Chengdu 610081, China;
3. College of Earth Science, Chengdu University of Technology, Chengdu 610059, China

Received:2019-11-20 Online:2020-09-26 Published:2020-09-29
Supported by:
Supported by National Natural Science Foundation of China (41702080, 91955208, 41602214), Project of China Geological Survey (DD20190644, DD20190147), Key Project of Science and Technology Support Program of the Ministry of Science and Technology of China (2016YFC060308, 2018YFC0604103)

摘要/Abstract

摘要： 藏南扎西康铅锌多金属矿床是特提斯喜马拉雅构造带（TH）东段发现的首个大型铅锌矿床，但其成因备受争议。本文在详细研究矿床地质特征的基础上，对矿硐内具有"同心环带"或"热水蛋"构造的铅锌矿石中的黄铁矿、方铅矿和闪锌矿进行了原位微区硫同位素分析。结果显示：铅锌矿石硫同位素组成变化范围在8.88‰~11.83‰之间，平均为10.50‰，总硫同位素组成（δ³⁴S_∑S）约为10.07‰。其中：7个黄铁矿（Py）测点的δ³⁴S_Py值为10.29‰~11.14‰，平均为10.70‰；6个闪锌矿（Sp）测点的δ³⁴S_Sp值为10.78‰~11.83‰，平均为11.49‰；5个方铅矿（Gn）测点的δ³⁴S_Gn值为8.88‰~9.18‰，平均为9.04‰。总体表现为δ³⁴S_Sp > δ³⁴S_Py > δ³⁴S_Gn，指示硫同位素未达到分馏平衡。利用方铅矿与闪锌矿矿物对硫同位素温度计计算可得，铅锌成矿温度介于224~280℃之间，平均值为259℃。结合前人研究成果，进一步得出扎西康铅锌多金属矿床主成矿期硫源主要来自日当组（J₁r）围岩地层，并可能有少量岩浆硫的混入，属受控于地层-构造-岩浆热液作用的中温热液矿床。

关键词: 原位硫同位素, 矿床成因, 中温热液矿床, 扎西康铅锌多金属矿床, 藏南

Abstract: Zhaxikang Pb-Zn polymetallic deposit is the first large-scale Pb-Zn deposit discovered in the eastern Tethys Himalaya (TH), but its genesis is still controversial. Based on the detailed study of the geological characteristics, the authors analyzed the in situ S isotope of pyrite, galena, and sphalerite in the Pb-Zn ore with "concentric ring zone" or "hot water egg" structure in the mine chamber. The results of in situ S isotopic analysis show that the isotopic composition of Pb-Zn ore varies from 8.88‰ -11.83‰, with an average of 10.50‰, and the total sulfur isotopic composition (δ³⁴S_∑S) is about 10.07‰. Among them, the δ³⁴S_Py of seven pyrite measuring points is 10.29‰-11.14‰, with an average of 10.70‰;the δ³⁴S_Sp of six sphalerite measuring points is 10.78‰-11.83‰, with an average of 11.49‰;and the δ³⁴S_Gn of five galena measuring points is 8.88‰-9.18‰, with an average of 9.04‰. It shows a trend of δ³⁴S_Sp > δ³⁴S_Py > δ³⁴S_Gn, indicating a status of fractionation disequilibrium. Using S isotope thermometer between galena and sphalerite, the Pb-Zn mineralization temperature is constrained between 224 ℃ and 280 ℃ with an average of 259 ℃. Combined with the results of previous studies, it is concluded that the sulfur source of Zhaxikang Pb-Zn polymetallic deposit is mainly from the surrounding strata of Ridang Formation (J₁r) with minor magma sulfur, and Zhaxikang Pb-Zn polymetallic deposit belongs to the filling metasomatic mesothermal deposit controlled by the stratigraphic, tectonic and magmatic hydrothermal processes.

Key words: in situ S isotopes, deposit genesis, mesothermal hydrothermal deposit, Zhaxikang Pb-Zn polymetallic deposit, southern Tibet

中图分类号:

李洪梁, 李光明, 丁俊, 张志, 卿成实, 付建刚, 凌晨, 刘宇奇. 藏南扎西康铅锌多金属矿床成因——硫化物原位硫同位素证据[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1289-1303.

Li Hongliang, Li Guangming, Ding Jun, Zhang Zhi, Qing Chengshi, Fu Jiangang, Ling Chen, Liu Yuqi. Genesis of Zhaxikang Pb-Zn Polymetallic Deposit in Southern Tibet: Evidence from in Situ S Isotopes of Sulfides[J]. Journal of Jilin University(Earth Science Edition), 2020, 50(5): 1289-1303.

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藏南扎西康铅锌多金属矿床成因——硫化物原位硫同位素证据

Genesis of Zhaxikang Pb-Zn Polymetallic Deposit in Southern Tibet: Evidence from in Situ S Isotopes of Sulfides

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