Late Neoproterozoic/Cambrian high-pressure mafic granulites from the Grove Mountains, East Antarctica: P-T-t path, collisional orogeny and implications for assembly of East Gondwana
The Grove Mountains are an inland continuation of the Late Neoproterozoic/Cambrian Prydz Belt of East Antarctica. In this paper we report high-pressure (HP) mafic granulites that occur in glacial moraines from this area. Petrographical textures, mineral compositions and P-T pseudosection calculation...
Published in: | Precambrian Research |
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Main Authors: | , , , , , |
Other Authors: | , , , , |
Format: | Journal/Newspaper |
Language: | English |
Published: |
precambrian research
2009
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11897/246241 https://doi.org/10.1016/j.precamres.2009.07.001 |