He, Ar, and S isotopic constraints on the relationship between A-type granites and tin mineralization: A case study of tin deposits in the Tengchong-Lianghe tin belt, southwest China | |
Xiao-Cui Chen; Cheng-Hai Zhao; Jing-Jing Zhu; Xin-Song Wang; Tao Cui | |
2018 | |
Source Publication | Ore Geology Reviews
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Volume | 92Pages:416-429 |
Abstract | The Tengchong-Lianghe tin belt in western Yunnan Province, southwest China, is the most important tin mineralization belt in the Sanjiang Tethyan Metallogenic Domain (STMD). There are two large tin deposits in this belt: the Paleogene Lailishan and the Late Cretaceous Xiaolonghe deposits. The two deposits are spatially and temporally associated with the Lailishan and Xiaolonghe granitic plutons, respectively. Recent studies suggest that the Lailishan and Xiaolonghe granitic plutons exhibit most of the mineralogical and geochemical characteristics of A-type granites. In this study, we discuss the He, Ar, and S isotopes of pyrite samples from the two large tin deposits to trace ore-forming fluids and elements. We also review the relationship between A-type granites and tin deposits from a new perspective. The delta S-34(CDT) values of the Lailishan tin deposit range from +4.9 parts per thousand to + 6.7 parts per thousand, with an average value of +5.53 parts per thousand. The delta S-34(CDT), values of the Xiaolonghe tin deposit range from + 5.0 parts per thousand to +8.1 parts per thousand, with an average value of +6.33 parts per thousand. These values are slightly higher than those of the granites (0 parts per thousand to + 5.7 parts per thousand) in the Tengchong-Lianghe area, indicating mainly magmatic sources for the sulfur of ore-forming fluids with a small amount of S from the wall rocks. The Lailishan tin deposit has He-3/He-4 values of 1.57-3.46 Ra, with an average value of 2.078 Ra, and Ar-40/Ar-36 values of 382.00-622.99, with an average value of 459.67. The Xiaolonghe tin deposit has He-3/He-4 values of 0.53-0.88 Ra, with an average value of 0.686 Ra, and Ar-40/Ar-36 values of 301.06-348.43, with an average value of 322.04. These values suggest that ore-forming fluids of the Lailishan and Xiaolonghe tin deposits have mixed crustal, mantle, and a small volume of meteoric water sources in different proportions. The mantle He-4 values and He-3/He-4 values of the Lailihsan tin deposit (26-44%, 1.57-3.46 Ra) are markedly higher than those of the Xiaolonghe tin deposit (8-15%, 0.53-0.88 Ra), implying increased crust-mantle interaction in the Paleogene relative to the Late Cretaceous in western Yunnan. This interaction may be attributed to the upwelling of the asthenosphere through the break-off of the Neo-Tethyan slab during the main collisional period (65-41 Ma) of India-Asia. |
Keyword | Tengchong–lianghe Tin Belt he, Ar, And s Isotopes ore-forming Fluids a-type Granite |
Indexed By | SCI |
Language | 英语 |
Document Type | 期刊论文 |
Identifier | http://ir.gyig.ac.cn/handle/42920512-1/8666 |
Collection | 矿床地球化学国家重点实验室 |
Affiliation | 1.Guizhou Institute of Technology, Guiyang 550003, China 2.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550005, China |
Recommended Citation GB/T 7714 | Xiao-Cui Chen;Cheng-Hai Zhao;Jing-Jing Zhu;Xin-Song Wang;Tao Cui. He, Ar, and S isotopic constraints on the relationship between A-type granites and tin mineralization: A case study of tin deposits in the Tengchong-Lianghe tin belt, southwest China[J]. Ore Geology Reviews,2018,92:416-429. |
APA | Xiao-Cui Chen;Cheng-Hai Zhao;Jing-Jing Zhu;Xin-Song Wang;Tao Cui.(2018).He, Ar, and S isotopic constraints on the relationship between A-type granites and tin mineralization: A case study of tin deposits in the Tengchong-Lianghe tin belt, southwest China.Ore Geology Reviews,92,416-429. |
MLA | Xiao-Cui Chen;Cheng-Hai Zhao;Jing-Jing Zhu;Xin-Song Wang;Tao Cui."He, Ar, and S isotopic constraints on the relationship between A-type granites and tin mineralization: A case study of tin deposits in the Tengchong-Lianghe tin belt, southwest China".Ore Geology Reviews 92(2018):416-429. |
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