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Mafic-ultramafic Intrusions in Beishan and Eastern Tianshan at Southern CAOB: Petrogenesis, Mineralization and Tectonic Implication (Hardcover, 2014 ed.)
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Mafic-ultramafic Intrusions in Beishan and Eastern Tianshan at Southern CAOB: Petrogenesis, Mineralization and Tectonic Implication (Hardcover, 2014 ed.)
Series: Springer Theses
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The widespread mafic-ultramafic complexes in the Earth are
well-known as their hosting Ni-Cu-PGE ore deposits, and their
petrogenesis and mineralization have become hot issues in the
geological studies. This thesis comprehensively investigated the
petrology, mineralogy, geochemistry and geochronology of several
mafic-ultramafic complexes in the Beishan Terrane, southern Central
Asian Orogenic Belt aimed at systematically determining the
mineralization and petrogenetic processes responsible for the
formation of the complexes and placing constraints on the tectonic
evolution of the Eastern Tianshan and Beishan, and the Early
Permian mantle plume. The thesis identified mineralizing indicators
of Ni-Cu sulfide deposits and defined the roles of partial melting,
fractional crystallization, crustal assimilation and magma
injection. The systematical isotopic compositions revealed the
mantle source of the mafic-ultramafic complexes had undergone the
subduction-related modifications both from the South Tianshan Ocean
and subsequently the Junggar Ocean, and that the complexes were
emplaced in the period of 269-285 Ma coeval with the 280 Ma mantle
plume event in the Tarim Craton. The results of this thesis provide
new insights about the tectonic setting, magma evolution, ore
genesis, and exploration implications of the mafic-ultramafic
complexes in Central Asian Orogenic Belt. Dr. Benxun Su works at
the Institute of Geology and Geophysics, Chinese Academy of
Sciences, China.
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