2021
DOI: 10.1016/j.oregeorev.2020.103971
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Iron and sulfur isotopes of sulfides from the Wocan hydrothermal field on the Carlsberg Ridge, Indian Ocean

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Cited by 12 publications
(1 citation statement)
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“…19,22,34,35 More recently, the Fe isotopic composition of pyrite is suggested to shed light on the formation of various types of sulde ore deposits, including magmatic-hydrothermal Sn-W deposits, 36 hydrothermal Au deposits, [37][38][39] porphyry Cu (-Mo) deposits, [40][41][42][43] skarn Cu-Fe deposits, 44 epigenetic sediment-hosted Cu-Co deposits, 45 sediment-hosted stratiform sulde deposits, 46 and sulde deposits on the modern seaoor. [47][48][49] The chemical zoning of pyrite can record a wealth of information during magma evolution and metamorphic reaction (e.g., ref. 33, 50 and 51).…”
Section: Introductionmentioning
confidence: 99%
“…19,22,34,35 More recently, the Fe isotopic composition of pyrite is suggested to shed light on the formation of various types of sulde ore deposits, including magmatic-hydrothermal Sn-W deposits, 36 hydrothermal Au deposits, [37][38][39] porphyry Cu (-Mo) deposits, [40][41][42][43] skarn Cu-Fe deposits, 44 epigenetic sediment-hosted Cu-Co deposits, 45 sediment-hosted stratiform sulde deposits, 46 and sulde deposits on the modern seaoor. [47][48][49] The chemical zoning of pyrite can record a wealth of information during magma evolution and metamorphic reaction (e.g., ref. 33, 50 and 51).…”
Section: Introductionmentioning
confidence: 99%