Results 161 to 170 of about 1,165,786 (215)

Mercury isotope evidence for the importance of recycled fluids in collisional ore systems. [PDF]

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Xu B   +7 more
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Transient non-soluble noble metal transport in hydrothermal ore systems. [PDF]

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Cano N   +4 more
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Petrogenesis of the granitoids related to skarn-type mineralization in the Nyainqentanglha Metallogenic Belt, Tibet. [PDF]

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Yangang F   +6 more
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Quantification of modal mineralogy in molybdenite-bearing drill-core samples by laser-induced breakdown spectroscopy. [PDF]

open access: yesHeliyon
Álvarez J   +5 more
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Oxygen Fugacity and Porphyry Mineralization: A Zircon Perspective of Dexing Porphyry Cu Deposit, China

Geochimica Et Cosmochimica Acta, 2017
Abstract Oxygen fugacity (fO2) is a key factor that controls the formation of porphyry Cu deposits. Porphyry Cu deposits are typically oxidized, but when and how porphyry magmas gain their high oxygen fugacity signatures, and how oxygen fugacity controls porphyry mineralization, remains obscure.
Saijun Sun, Wei-Dong Sun, Li-Peng Zhang
exaly   +2 more sources

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