Textures and mineral compositions of the Xinjie layered intrusion, SW China: Implications for the origin of magnetite and fractionation process of Fe-Ti-rich basaltic magmas

Textures and mineral compositions of the Xinjie layered intrusion, SW China: Implications for the origin of magnetite and fractionation process of Fe-Ti-rich basaltic magmas

The Xinjie layered intrusion in the Panxi region, SW China, hosts both Fe-Ti oxide and platinum-group element (PGE) sulfide mineralization. The intrusion can be divided, from the base upward, into Units I, II and III, in terms of mineral assemblages. Units I and II are mainly composed of wehrlite an...

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Bibliographic Details
Main Authors: Huan Dong, Changming Xing, Christina Yan Wang
Format: Article
Language:English
Published: Elsevier 2013-09-01
Series:Geoscience Frontiers
Subjects:
Geochemistry
Fe-Ti oxides
Mineral composition
The Xinjie layered mafic-ultramafic intrusion
Emeishan large igneous province
Online Access:http://www.sciencedirect.com/science/article/pii/S1674987113000303

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http://www.sciencedirect.com/science/article/pii/S1674987113000303

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