Genesis of the Linghu Au deposit in Xiaoqinling Region, Henan province, China: Constraints from fluid inclusions and iso
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ORIGINAL PAPER
Genesis of the Linghu Au deposit in Xiaoqinling Region, Henan province, China: Constraints from fluid inclusions and isotope systematics Wei Zeng 1,2 & Zhi-gao Wang 1 & Duo Wan 1 & Feng-yue Sun 1 & Cheng-dong Li 2 & Reng-an Yu 2 & Jia-ying Wang 2 & Jian-chang Xu 3 Received: 17 January 2019 / Accepted: 20 August 2020 # Saudi Society for Geosciences 2020
Abstract The Linghu Au deposit is located within the northeastern part of the Xiaoqinling region in the southern margin of the North China Craton. Field investigations, cross-cutting relationships, and mineral paragenetic associations have identified three stages of hydrothermal activity. To determine the origin and evolution of ore-forming fluids, and better understand genesis of the Linghu Au deposit, we have undertaken a series of studies including fluid inclusion and He–Ar–H–O–S–Pb isotope systematics. Fluid inclusion study indicates that the early stage of gold mineralization was characterized by a hightemperature and low-salinity H 2O–CO 2–NaCl hydrothermal fluids that have δD values of – 82.0 to – 78.6‰ and δ18OH2O values of 5.3 to 6.4‰. The intermediate stage of gold mineralization involved moderate temperature H2O– CO2–NaCl hydrothermal fluids with δD and δ18OH2O values of – 92.7‰ to – 87.9‰ and – 1.4‰ to 0‰, respectively. Pyrite samples from this mineralization stage have 3He/4He and 40Ar/36Ar ratios of 0.26–0.31 Ra and 2834.7–4300.6, respectively. The last mineralization stage involved (low-temperature and low-salinity NaCl–H2O system of hydrothermal fluids with relatively lower δD values of – 93.1 to – 92.3‰ and δ18OH2O values of – 5.7 to – 5.2‰. Moreover, sulfides in ores yielded δ34S values of – 3.6 to 5.9‰, with an average of 2.65‰. The sulfides have 206Pb/204Pb ratios of 17.101– 17.804, 207Pb/204Pb ratios of 15.438–15.554, and 208Pb/204Pb ratios of 37.438–38.654. The results of fluid inclusions and H–O, S–Pb, and He–Ar isotopes indicate that hydrothermal fluids associated with the early stage of mineralization originated from magmatic fluids, with sulfur and lead being derived from both units of the Taihua Group and a Late Triassic magmatic–hydrothermal system. All of these data indicate that the Linghu gold deposit formed as a result of magmatic– hydrothermal mineralizing processes. Keywords Linghu Au deposit . H . O . S . Pb isotopes . Pyrite He . Ar . Fluid inclusions . Xiaoqinling region
Responsible Editor: Amjad Kallel * Wei Zeng [email protected]
Reng-an Yu [email protected] Jian-chang Xu [email protected]
Zhi-gao Wang [email protected] Duo Wan [email protected]
1
College of Earth Sciences, Jilin University, Changchun 130061, China
Feng-yue Sun [email protected]
2
Tianjin Center, China Geological Survey, Tianjin 300170, China
3
No 1 Institute of Geological and Mineral Resources Survey, Henan Geological Bureau, Luoyang 471023, China
Cheng-dong Li [email protected]
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Introduction The Xiaoqinling area is located within the southern margin of the North China Craton and forms part of the Qinling–Dabie o
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