In situ SIMS U-Pb dating of hydrothermal rutile: reliable age for the Zhesang Carlin-type gold deposit in the golden triangle region, SW China
Autor: | Richen Zhong, Bin Xiong, Ruizhong Hu, Qiaohui Pi, Qiu-Li Li |
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Rok vydání: | 2017 |
Předmět: |
Isochron
Arsenopyrite Mineralization (geology) 010504 meteorology & atmospheric sciences Pluton Geochemistry Mineralogy 010502 geochemistry & geophysics 01 natural sciences Hydrothermal circulation Geophysics Geochemistry and Petrology Rutile visual_art visual_art.visual_art_medium Economic Geology Radiometric dating Carlin–type gold deposit Geology 0105 earth and related environmental sciences |
Zdroj: | Mineralium Deposita. 52:1179-1190 |
ISSN: | 1432-1866 0026-4598 |
DOI: | 10.1007/s00126-017-0715-y |
Popis: | The contiguous region between Guangxi, Guizhou, and Yunnan, commonly referred to as the Golden Triangle region in SW China, hosts many Carlin-type gold deposits. Previously, the ages of the gold mineralization in this region have not been well constrained due to the lack of suitable minerals for radiometric dating. This paper reports the first SIMS U–Pb age of hydrothermal rutile crystals for the Zhesang Carlin-type gold deposit in the region. The hydrothermal U-bearing rutile associated with gold-bearing sulfides in the deposit yields an U-Pb age of 213.6 ± 5.4 Ma, which is within the range of the previously reported arsenopyrite Re–Os isochron ages (204 ± 19 to 235 ± 33 Ma) for three other Carlin-type gold deposits in the region. Our new and more precise rutile U-Pb age confirms that the gold mineralization was contemporaneous with the Triassic W–Sn mineralization and associated granitic magmatism in the surrounding regions. Based on the temporal correlation, we postulate that coeval granitic plutons may be present at greater depths in the Golden Triangle region and that the formation of the Carlin-type gold deposits is probably linked to the coeval granitic magmatism in the region. This study clearly demonstrates that in situ rutile U–Pb dating is a robust tool for the geochronogical study of hydrothermal deposits that contain hydrothermal rutile. |
Databáze: | OpenAIRE |
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