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...
Published in: | Journal of Asian Earth Sciences |
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Main Authors: | , , , , , |
Format: | Report |
Language: | English |
Published: |
PERGAMON-ELSEVIER SCIENCE LTD
2017
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Subjects: | |
Online Access: | http://ir.gig.ac.cn/handle/344008/45379 https://doi.org/10.1016/j.jseaes.2017.06.012 |