Ultramafic to mafic granulites from the Larsemann Hills, East Antarctica: Geochemistry and tectonic implications

The Larsemann Hills area is part of a reworked early Neoproterozoic metamorphic terrain in southwestern Prydz Bay, East Antarctica. Ultramafic and mafic granulites, whose origins remain controversial, occur as lenses, boudins or layered bodies within the para- and ortho-gneiss in the region. The ult...

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Bibliographic Details
Published in:Journal of Asian Earth Sciences
Main Authors: Tong, Laixi, Jahn, Bor-ming, Liu, Xiaohan, Liang, Xirong, Xu, Yi-gang, Ionov, Dmitri
Format: Report
Language:English
Published: PERGAMON-ELSEVIER SCIENCE LTD 2017
Subjects:
Online Access:http://ir.gig.ac.cn/handle/344008/45379
https://doi.org/10.1016/j.jseaes.2017.06.012