Magma oxygen fugacity of mafic-ultramafic intrusions in convergent margin settings: Insights for the role of magma oxidation states on magmatic Ni-Cu sulfide mineralization
Abstract
Oxygen fugacities
Ni-Cu sulfide-bearing mafic-ultramafic intrusions in the CAOB include arc-related Silurian-Carboniferous ones and post-collisional Permian-Triassic ones. Arc-related intrusions formed before the closure of the paleo-Asian ocean and include the Jinbulake, Heishan, Kuwei, and Erbutu intrusions. Post-collisional intrusions were emplaced in extensional settings after the closure of the paleo-Asian ocean and include the Kalatongke, Baixintan, Huangshandong, Huangshan, Poyi, Poshi, Tulaergen, and Hongqiling No. 7 intrusions. It is clear that the magma
Acknowledgments and Funding
S. Yang provided the samples of the Jinbulake intrusion and B. Su shared the EPMA data for the olivine and spinel of the Luodong intrusion. Constructive reviews by A. Tomkins and an anonymous reviewer have greatly improved the quality of this manuscript. This work was supported by grants from the National Natural Science Foundation of China (No. 41730423 and 41902077), and China Postdoctoral Science Foundation Grant (No. 2019M653103).
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Artikel in diesem Heft
- MSA Centennial Review Paper
- The incompressibility of atoms at high pressures
- Phase transitions in Ɛ-FeOOH at high pressure and ambient temperature
- Thermal state of the upper mantle and the origin of the Cambrian-Ordovician ophiolite pulse: Constraints from ultramafic dikes of the Hayachine-Miyamori ophiolite
- Quadrivalent praseodymium in planetary materials
- Quantitative microscale Fe redox imaging by multiple energy X-ray fluorescence mapping at the Fe K pre-edge peak
- Quantification of excess 231Pa in late Quaternary igneous baddeleyite
- Magma oxygen fugacity of mafic-ultramafic intrusions in convergent margin settings: Insights for the role of magma oxidation states on magmatic Ni-Cu sulfide mineralization
- Investigation of the crystal structure of a low water content hydrous olivine to 29.9 GPa: A high-pressure single-crystal X-ray diffraction study
- Ferric-ferrous iron ratios of experimental majoritic garnet and clinopyroxene as a function of oxygen fugacity
- The origin of Ti-oxide minerals below and within the eastern Athabasca Basin, Canada
- Partition behavior of platinum-group elements during the segregation of arsenide melts from sulfide magma
- Vapor-bubble growth in olivine-hosted melt inclusions
- New Mineral Names
Artikel in diesem Heft
- MSA Centennial Review Paper
- The incompressibility of atoms at high pressures
- Phase transitions in Ɛ-FeOOH at high pressure and ambient temperature
- Thermal state of the upper mantle and the origin of the Cambrian-Ordovician ophiolite pulse: Constraints from ultramafic dikes of the Hayachine-Miyamori ophiolite
- Quadrivalent praseodymium in planetary materials
- Quantitative microscale Fe redox imaging by multiple energy X-ray fluorescence mapping at the Fe K pre-edge peak
- Quantification of excess 231Pa in late Quaternary igneous baddeleyite
- Magma oxygen fugacity of mafic-ultramafic intrusions in convergent margin settings: Insights for the role of magma oxidation states on magmatic Ni-Cu sulfide mineralization
- Investigation of the crystal structure of a low water content hydrous olivine to 29.9 GPa: A high-pressure single-crystal X-ray diffraction study
- Ferric-ferrous iron ratios of experimental majoritic garnet and clinopyroxene as a function of oxygen fugacity
- The origin of Ti-oxide minerals below and within the eastern Athabasca Basin, Canada
- Partition behavior of platinum-group elements during the segregation of arsenide melts from sulfide magma
- Vapor-bubble growth in olivine-hosted melt inclusions
- New Mineral Names