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

Autor: LIU, Y.G., LI, W.Y., LÜ, X.B., HUO, Y.H., ZHANG, B.

Publikováno v: Geologica Acta; Vol. 15 No 1 (2017); 37-50, I-III
Geologica Acta; Vol. 15 No. 1 (2017); 37-50, I-III
Geologica Acta; Vol. 15 Núm. 1 (2017); 37-50, I-III
RCUB. Revistas Científicas de la Universidad de Barcelona
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Geologica Acta; 2017: Vol.: 15 Núm.: 1; p. 37-50, I-III

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 f

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https://revistes.ub.edu/index.php/GEOACTA/article/view/GeologicaActa2017.15.1.4