Geochronology and geochemistry of the Banjiaoyuan tin deposit, southern Hunan Province and its geological implications
[Display omitted] •Precisely determined the metallogenic age of Banjiaoyuan tin deposit.•Analyzed the origin of ore-forming fluid.•Discussed the elemental substitution mechanism and precipitation of cassiterites in Banjiaoyuan tin deposit. Situated in the central part of the Southern Hunan segment o...
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Published in | Ore geology reviews Vol. 168; p. 106038 |
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Main Authors | , , , , , , , , , |
Format | Journal Article |
Language | English |
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Elsevier B.V
01.05.2024
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Abstract | [Display omitted]
•Precisely determined the metallogenic age of Banjiaoyuan tin deposit.•Analyzed the origin of ore-forming fluid.•Discussed the elemental substitution mechanism and precipitation of cassiterites in Banjiaoyuan tin deposit.
Situated in the central part of the Southern Hunan segment of the Nanling Metallogenic Belt, the Banjiaoyuan tin deposit represents a significant Indosinian quartz vein type tin deposit. Based on field geological surveys and petrographic observations, the mineralization in the area can be divided into three stages: (I) early greisen stage, (II) cassiterite-quartz vein stage, and (III) late barren quartz vein stage. The dating results show that the 40Ar-39Ar plateau age of muscovite in stage I is 215.51 ± 0.87 Ma, and the Rb-Sr isochronous age of quartz mineral in stage II is 214.2 ± 3.1 Ma (MSWD = 1.3), both of which are coincide with the cassiterite U-Pb lower intercept age (215.7 ± 1.3 Ma, MSWD = 1.2), confirming the existence of metallogenic events in this region during the late Indosinian. The δD and δ18O of quartz in stage II range from −66.2 to −80.2 ‰, and 3.71 to 6.17 ‰, respectively, indicating that the ore-forming fluid is mainly derived from a mixture of magmatic-hydrothermal fluids and a small amount of meteoric water. We applied LA-ICP-MS chemical mapping and trace elements analysis to cassiterites, found that they underwent a transition from oxidation to reduction during precipitation when the fluids tend to be more volatile-rich and highly fractionated. The formation of the Banjiaoyuan tin deposit is closely related to the late Indosinian magmatic activity in the Yangmingshan region. Besides, the deep and peripheral parts of the mining area also have the potential for large-scale vein-type and greisen-type W-Sn mineralization. |
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AbstractList | [Display omitted]
•Precisely determined the metallogenic age of Banjiaoyuan tin deposit.•Analyzed the origin of ore-forming fluid.•Discussed the elemental substitution mechanism and precipitation of cassiterites in Banjiaoyuan tin deposit.
Situated in the central part of the Southern Hunan segment of the Nanling Metallogenic Belt, the Banjiaoyuan tin deposit represents a significant Indosinian quartz vein type tin deposit. Based on field geological surveys and petrographic observations, the mineralization in the area can be divided into three stages: (I) early greisen stage, (II) cassiterite-quartz vein stage, and (III) late barren quartz vein stage. The dating results show that the 40Ar-39Ar plateau age of muscovite in stage I is 215.51 ± 0.87 Ma, and the Rb-Sr isochronous age of quartz mineral in stage II is 214.2 ± 3.1 Ma (MSWD = 1.3), both of which are coincide with the cassiterite U-Pb lower intercept age (215.7 ± 1.3 Ma, MSWD = 1.2), confirming the existence of metallogenic events in this region during the late Indosinian. The δD and δ18O of quartz in stage II range from −66.2 to −80.2 ‰, and 3.71 to 6.17 ‰, respectively, indicating that the ore-forming fluid is mainly derived from a mixture of magmatic-hydrothermal fluids and a small amount of meteoric water. We applied LA-ICP-MS chemical mapping and trace elements analysis to cassiterites, found that they underwent a transition from oxidation to reduction during precipitation when the fluids tend to be more volatile-rich and highly fractionated. The formation of the Banjiaoyuan tin deposit is closely related to the late Indosinian magmatic activity in the Yangmingshan region. Besides, the deep and peripheral parts of the mining area also have the potential for large-scale vein-type and greisen-type W-Sn mineralization. |
ArticleNumber | 106038 |
Author | Zhang, Tuyan Hu, Tianyang Lu, Youyue Fu, Jianming Du, Yun Zhang, Kun Xu, Guofeng Dai, Pingyun Zhang, Zunzun Liu, Lei |
Author_xml | – sequence: 1 givenname: Zunzun surname: Zhang fullname: Zhang, Zunzun organization: Wuhan Centre, China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China – sequence: 2 givenname: Guofeng surname: Xu fullname: Xu, Guofeng organization: Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, School of Geosciences and Info-Physics, Central South University, Changsha 410083, China – sequence: 3 givenname: Youyue surname: Lu fullname: Lu, Youyue organization: Wuhan Centre, China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China – sequence: 4 givenname: Lei surname: Liu fullname: Liu, Lei email: liu01@ustc.edu.cn organization: Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, School of Geosciences and Info-Physics, Central South University, Changsha 410083, China – sequence: 5 givenname: Tianyang surname: Hu fullname: Hu, Tianyang organization: Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, School of Geosciences and Info-Physics, Central South University, Changsha 410083, China – sequence: 6 givenname: Tuyan surname: Zhang fullname: Zhang, Tuyan organization: CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China – sequence: 7 givenname: Yun surname: Du fullname: Du, Yun organization: Hunan Institute of Geological Survey, Changsha, Hunan 410116, China – sequence: 8 givenname: Jianming surname: Fu fullname: Fu, Jianming organization: Wuhan Centre, China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China – sequence: 9 givenname: Kun surname: Zhang fullname: Zhang, Kun organization: Wuhan Centre, China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China – sequence: 10 givenname: Pingyun surname: Dai fullname: Dai, Pingyun organization: Wuhan Centre, China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China |
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Keywords | Muscovite Ar-Ar dating Nanling metallogenic belt Quartz vein type tin ore Rb-Sr dating of quartz LA-ICP-MS chemical mapping of cassiterite |
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Title | Geochronology and geochemistry of the Banjiaoyuan tin deposit, southern Hunan Province and its geological implications |
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