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Appendix B. Origin of Fe–Ni–Cu (Co) sulfide and Fe–Ti oxide minerals in the c. 1.77 Ga dolerite dyke, Singhbhum Craton (eastern India)

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posted on 2021-10-01, 11:25 authored by Arnab Dey, Sisir K. Mondal
EPMA of titanomagnetite and ilmenite

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    Geological Society, London, Special PublicationsGeological Society, London, Special Publications

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    singhbhum cratoneastern indiac appendix bGeology

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