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- W1569416761 abstract "The Habo South porphyry Cu-Au-(Mo) deposit, China, occurs in a series of granitic intrusions that have been overprinted by extensive K-feldspar-biotite alteration. Veins of quartz, quartz-magnetite, quartz-biotite, and sulfides occur widely. Several igneous phases have been affected by the mineralization, and host rock textures indicate that all phases were saturated with volatiles. A formation age of 36-34 Ma has been obtained by ELA-ICPMS on zircons from the deposit. This suggests a trend to younger ages of porphyries along the Red River Fault Zone. Average Ce4+/Ce3+ ratios of 240 (with some to >1000) imply highly oxidized and evolved magmas, consistent with intrusions related to porphyry systems elsewhere along the Red River Fault Zone." @default.
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- W1569416761 date "2007-01-01" @default.
- W1569416761 modified "2023-09-26" @default.
- W1569416761 title "Fluid Saturation in the Habo South Porphyry Cu-Au (Mo) System, Southern China: Application of Petrology to Mineral Exploration." @default.
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