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The genetic relationship between the large Guanfang W deposit and granitic intrusions, in Yunnan Province, southwest China: Evidence from UPb and ReOs geochronology and Pb and Sr isotopic characteristics
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文摘

The intrusion of Suozuodi granite and W mineralization at the Guanfang Deposit took place simultaneously at ca. 92 Ma.

The ore-forming materials of Guanfang deposit were derived from a crustal source, without addition mantle materials.

Formation of Guanfang W deposit were related to collisional tectonic setting.

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