Magmatic evolution and tectonic setting of metabasites from Lützow-Holm Complex, East Antarctica

Metabasites from the Lützow-Holm Complex, East Antarctica, are the equivalent of metamorphosed ultramafic and mafic rocks with ultrabasic to intermediate compositions, which occur as layers and blocks in the quartzo-feldspathic or metasedimentary gneisse

Bibliographic Details
Published in:Geological Society, London, Special Publications
Main Authors: Suda, Yoshimitsu, Kawano, Yoshinobu, Yaxley, Gregory, Korenaga, Hiroshi, Hiroi, Yoshikuni
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of London
Subjects:
Keywords: continental crust
cumulate
feldspar
geochemistry
gneiss
Gondwana
island arc
mafic rock
metabasite
metamorphic rock
metamorphism
neodymium isotope
Pan African orogeny
protolith
seafloor
subduction
tectonic setting
ultramafic rock
Antarcti
East Antarctica
Antarc*
Antarctica
Online Access:http://hdl.handle.net/1885/37682
https://doi.org/10.1144/SP308.11
https://openresearch-repository.anu.edu.au/bitstream/1885/37682/5/YaxleyGM_RSES_2008_Suda_Magmatic_evolution.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/37682/7/01_Suda_Magmatic_evolution_and_2008.pdf.jpg
Description
Summary:Metabasites from the Lützow-Holm Complex, East Antarctica, are the equivalent of metamorphosed ultramafic and mafic rocks with ultrabasic to intermediate compositions, which occur as layers and blocks in the quartzo-feldspathic or metasedimentary gneisse

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