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

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

Description

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

CollectionsANU Research Publications
Date published: 2012
Type: Journal article
URI: http://hdl.handle.net/1885/63067
Source: International Geology Review
DOI: 10.1080/00206814.2010.543011

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