Mercury isotope evidence for the importance of recycled fluids in collisional ore systems. [PDF]
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Unveiling the metallogenic continuum of an Archean craton. [PDF]
Demmer M, Ezad I, Fiorentini M.
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Mining of primary raw materials as the critical foundation of 'sustainable' metals: a wicked problem for technology innovation clusters. [PDF]
Moore KR, Marquis E, Shanks K, Wall F.
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Transient non-soluble noble metal transport in hydrothermal ore systems. [PDF]
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Petrogenesis of the granitoids related to skarn-type mineralization in the Nyainqentanglha Metallogenic Belt, Tibet. [PDF]
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Quantification of modal mineralogy in molybdenite-bearing drill-core samples by laser-induced breakdown spectroscopy. [PDF]
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Source analysis and ecological risk assessment of potentially toxic elements in farmland soil around a mining area. [PDF]
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Gold geochemical anomalies delineated by the stratigraphic zoning anomaly lower limit contrast method: a case study of panjiaba, Shaanxi province, China. [PDF]
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Copper deposit development potential on the Qinghai-Xizang Plateau in China based on the pressure-state-response framework. [PDF]
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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.
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