Pre-metamorphis carbon, oxygen and strontium isotope signature of high-grade marbles from the Lutzow-Holm Complex, East Antarctica: apparent age constraints of carbonate deposition

C, O and Sr isotope geochemistry of high-grade marbles from the Lützow-Holm Complex, East Antarctica, has given clues on the depositional ages and post-depositional alterations. Dolomitic and calcitic marbles occur as thin layers with varying thickness (

Bibliographic Details
Published in:Geological Society, London, Special Publications
Main Authors: Satish-Kumar, M, Miyamoto, T, Hermann, Joerg, Kagami, Hiroo, Osanai, Y, Motoyoshi, Yoichi
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of London
Subjects:
Keywords: calcite
carbon isotope
carbonate
chemical alteration
deposition
depositional environment
diagenesis
dolomite
Gondwana
marble
metamorphism
outcrop
oxygen isotope
progradation
rare earth element
retrograde metamorphism
strontium isotope
Ant
East Antarctica
Antarc*
Antarctica
Online Access:http://hdl.handle.net/1885/55441
https://doi.org/10.1144/SP308.7
https://openresearch-repository.anu.edu.au/bitstream/1885/55441/5/GSL308_147_08.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/55441/7/01_Satish-Kumar_Pre-metamorphis_carbon,_oxygen_2008.pdf.jpg
Description
Summary:C, O and Sr isotope geochemistry of high-grade marbles from the Lützow-Holm Complex, East Antarctica, has given clues on the depositional ages and post-depositional alterations. Dolomitic and calcitic marbles occur as thin layers with varying thickness (

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