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Re–Os molybdenite and Ar–Ar phlogopite dating of Cu–Fe–Au–Mo (W) deposits in southeastern Hubei, China

The Cu-Fe-Au-Mo (W) deposits in southeastern Hubei are an important component of the Middle-Lower Yangtze River metallogenic belt. Molybdenite from the Fengshandong Cu- (Mo), Ruanjiawan W-Cu- (Mo), Qianjiawan Cu-Au, Tongshankou Cu-Mo and Tonglüshan Cu- (Fe) deposits yielded Re-Os ages of 144.0 ± 2.1...

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Published in:Mineralogy and petrology 2007-07, Vol.90 (3-4), p.249-270
Main Authors: Xie, G.-Q., Mao, J.-W., Li, R.-L., Qü, W.-J., Pirajno, F., Du, A.-D.
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description The Cu-Fe-Au-Mo (W) deposits in southeastern Hubei are an important component of the Middle-Lower Yangtze River metallogenic belt. Molybdenite from the Fengshandong Cu- (Mo), Ruanjiawan W-Cu- (Mo), Qianjiawan Cu-Au, Tongshankou Cu-Mo and Tonglüshan Cu- (Fe) deposits yielded Re-Os ages of 144.0 ± 2.1 Ma, 143.6 ± 1.7 Ma, 137.7 ± 1.7 Ma, 142.3 ± 1.8-143.7 ± 1.8 Ma and 137.8 ± 1.7-138.1 ± 1.8 Ma, respectively. Phlogopite from the Tieshan Fe- (Cu) deposit yielded an Ar-Ar age of 140.9 ± 1.2 Ma. These data and other published isotopic ages (Re-Os molybdenite and Ar-Ar mica ages) for the Cu-Fe-Au-Mo (W) deposits in the Middle-Lower Yangtze River metallogenic belt show that Cu-Fe-Au-Mo (W) mineralisation in the Tongling, Anqing, Jiurui and Edong ore districts developed in a narrow time span between 135.5 and 144.9 Ma, reflecting an important regional metallogenic event. An integrated study of available petrological and geochronological data, together with relationships to magmatism and the regional geodynamic framework, indicate that the Cu-Fe-Au-Mo (W) mineralisation in the Middle-Lower Yangtze River belt occurred during a regime of lithospheric extension. This extension is probably related to Late Mesozoic processes of lower crustal delamination and lithospheric thinning in East China. [PUBLICATION ABSTRACT]
doi_str_mv 10.1007/s00710-006-0176-y
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Molybdenite from the Fengshandong Cu- (Mo), Ruanjiawan W-Cu- (Mo), Qianjiawan Cu-Au, Tongshankou Cu-Mo and Tonglüshan Cu- (Fe) deposits yielded Re-Os ages of 144.0 ± 2.1 Ma, 143.6 ± 1.7 Ma, 137.7 ± 1.7 Ma, 142.3 ± 1.8-143.7 ± 1.8 Ma and 137.8 ± 1.7-138.1 ± 1.8 Ma, respectively. Phlogopite from the Tieshan Fe- (Cu) deposit yielded an Ar-Ar age of 140.9 ± 1.2 Ma. These data and other published isotopic ages (Re-Os molybdenite and Ar-Ar mica ages) for the Cu-Fe-Au-Mo (W) deposits in the Middle-Lower Yangtze River metallogenic belt show that Cu-Fe-Au-Mo (W) mineralisation in the Tongling, Anqing, Jiurui and Edong ore districts developed in a narrow time span between 135.5 and 144.9 Ma, reflecting an important regional metallogenic event. 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subjects Copper
Geochemistry
Geological time
Mesozoic
Mineralization
Mineralogy
Minerals
Petrology
Rivers
title Re–Os molybdenite and Ar–Ar phlogopite dating of Cu–Fe–Au–Mo (W) deposits in southeastern Hubei, China
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