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Thermochronologic constrains on the processes of formation and exhumation of the Xinli orogenic gold deposit, Jiaodong Peninsula, eastern China
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文摘
Ductile deformation on Sanshandao fault occurred before 124 Ma, after magmatism at ~ 129 Ma, and before gold mineralization Gold mineralization was associated with brittle, normal faulting and generalized brecciation on Sanshandao Fault at ~ 121 Ma Extension and normal faulting were responsible to little post-mineralization exhumation that preserved the deposit

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