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Geochronologic-petrochemical studies of the Hongshishan mafic-ultramafic intrusion, Beishan area, Xinjiang (NW China): Petrogenesis and tectonic implications

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Authors

Su, Ben-Xun
Qin, Ke-Zhang
Sakyi, Patrick Asamoah
Tang, Dong-Mei
Liu, Pingping
Malaviarachchi, Sanjeewa
Xiao, Qing-Hua
Sun, He

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V.H. Winston & Sons

Abstract

The Hongshishan mafic-ultramafic intrusion (SIMS zircon U-Pb age 286.4 ± 2.8Ma) consists of dunite, clinopyroxene peridotite, troctolite, and gabbro. Major elements display systematic correlations. Trace elements have identical distribution patterns, inc

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International Geology Review

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Restricted until

2037-12-31