The Pobei Cu-Ni and Fe ore deposits in NW China are comagmatic evolution products: evidence from ore microscopy, zircon U-Pb chronology and geochemistry

The Pobei Cu-Ni and Fe ore deposits in NW China are comagmatic evolution products: evidence from ore microscopy, zircon U-Pb chronology and geochemistry

The Pobei mafic-ultramafic complex in northwestern China comprises magmatic Cu-Ni sulfide ore deposits coexisting with Fe-Ti oxide deposits. The Poshi, Poyi, and Podong ultramafic intrusions host the Cu-Ni ore. The ultramafic intrusions experienced four stages during its formation. The intrusion se...

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Bibliographic Details
Main Authors: Y.G. LIU, W.Y. LI, X.B. LÜ, Y.H. HUO, B. ZHANG
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2017-02-01
Series:Geologica Acta
Subjects:
Magmatic Cu-Ni sulfide deposit
Xiaochangshan Fe deposit
Crystallization differentiation
Magnetite-mineralized gabbro
Beishan
Early Permian
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/16095

Internet

https://revistes.ub.edu/index.php/GEOACTA/article/view/16095

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