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Multiple-stage mineralization in the Sawayaerdun orogenic gold deposit, western Tianshan, Xinjiang: Constraints from paragenesis, EMPA analyses, Re-Os dating of pyrite (arsenopyrite) and U-Pb dating of zircon from the host rocks
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文摘
Three generations of auriferous pyrite (Py0, Py1 and Py2) have been recognized. U–Pb dating of detrital zircons constrained the maximum deposition age of 355.0 ± 7.3 Ma. Auriferous pyrite (arsenopyrite) Re–Os dating yielded the ages of 323.9 ± 4.8 Ma and 282 ± 12 Ma, respectively. Py1 is interpreted to have formed in the syn-tectonic stage and Py2 was formed during the late- to post-tectonic stage. Os isotopes of auriferous separates from the two stages point to crustal sources of the metals.

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