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- W1500052448 abstract "The Dongping gold deposit,situated on the northern margin of the North China Platform,is a composite deposit composed of auriferous quartz vein-type and altered rock-type ore bodies.It is hosted in the inner contact zone of an alkaline intrusion which was intruded in to Archean metamorphic rocks and was formed not later than the Hercynian period.Auriferous quartz veins of the deposit are dated with the fluid inclusion Rb-Sr isochron method at 103±4Ma ,indicating that the gold deposit was formed in the Yenshanian period,^86Sr/^86Sr source tracing shows the ore-forming materials came dominantly from alkaline intrusions.These results combined with other isotope and REE data,suggest that the Dongping gold deposit is not a traditiolal magmatic hydrothermal deposit,but a reworked hydrothermal deposit related to heated and evolved meteoric water." @default.
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- W1500052448 date "1996-01-01" @default.
- W1500052448 modified "2023-09-22" @default.
- W1500052448 title "Auriferous Quartz Veins from the Dongping Gold Deposit,NW Hebei Province and Metallogenesis—Fluid Inclusion Rb—Sr Isochron Evidence" @default.
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