Oxidation state inherited from the magma source and implications for mineralization: Late Jurassic to Early Cretaceous granitoids, Central Lhasa subterrane, Tibet

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Oxidation state inherited from the magma source and implications for mineralization: Late Jurassic to Early Cretaceous granitoids, Central Lhasa subterrane, Tibet

Arc magmas are more oxidized than mid-ocean ridge basalts; however, there is continuing debate as to whether this higher oxidation state is inherited from the source magma or developed during late-stage magmatic differentiation processes. Well-constrained Late Jurassic to Early Cretaceous arc-relate...

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Bibliographic Details
Main Authors:	Cao, Mingjian, Qin, K., Li, G., Evans, Noreen, McInnes, Brent, Li, J., Zhao, J.
Format:	Journal Article
Published:	Springer 2017
Online Access:	http://hdl.handle.net/20.500.11937/53122

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