Geochronological constraints on the Late Proterozoic to Cambrian crustal evolution of eastern Dronning Maud Land, East Antarctica: A synthesis of SHRIMP U-Pb age and Nd model age data

In eastern Dronning Maud Land (DML), East Antarctica, there are several discrete, isolated magmatic and high-grade metamorphic regions. These are, from west (c. 20°E) to east (c. 50°E), the Sør Rondane Mountains (SRM), Yamato-Belgica Complex (YBC), Lü

Bibliographic Details
Published in:Geological Society, London, Special Publications
Main Authors: Shiraishi, Kazuyuki, Dunkley, Daniel, Hokada, T., Fanning, Christopher, Kagami, Hiroo, Hamamoto, Takuji
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of London
Subjects:
Keywords: amphibolite facies
Archean
Cambrian
contact metamorphism
crustal evolution
geochronology
Gondwana
granitoid
granulite facies
Grenvillian orogeny
metamorphic rock
metasedimentary rock
neodymium
Pan African orogeny
plutonic rock
Proterozoic
East Antarctica
Dronning Maud Land
Yamato
Sør-Rondane
Sør Rondane Mountains
Antarc*
Antarctica
DML
Online Access:http://hdl.handle.net/1885/82547
https://doi.org/10.1144/SP308.2
https://openresearch-repository.anu.edu.au/bitstream/1885/82547/5/Fanning_2008_Dronning_Maud.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/82547/7/01_Shiraishi_Geochronological_constraints_2008.pdf.jpg
Description
Summary:In eastern Dronning Maud Land (DML), East Antarctica, there are several discrete, isolated magmatic and high-grade metamorphic regions. These are, from west (c. 20°E) to east (c. 50°E), the Sør Rondane Mountains (SRM), Yamato-Belgica Complex (YBC), Lü

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