Sulfide evolution in high-temperature to ultrahigh-temperature metamorphic rocks from Lutzow-Holm Complex, East Antarctica

The high-temperature (HT) to ultrahigh-temperature (UHT) metamorphic rocks from Lützow-Holm Complex, East Antarctica show a systematic difference between sulfide assemblages in the rock matrix and those found as inclusions in the silicates stable in high

Bibliographic Details
Published in:Lithos
Main Authors: Kawakami, Tetsuo, Ellis, David, Christy, Andrew
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier
Subjects:
Keywords: chalcopyrite
fluid inclusion
metamorphic rock
P-T-t path
pentlandite
pyrrhotite
solid solution
sulfide
ultrahigh temperature metamorphism
Antarctica
East Antarctica
Lutzow-Holm Bay Fluid
Inclusion
P-T path
UHT metamorphism
Antarc*
Online Access:http://hdl.handle.net/1885/17861
https://doi.org/10.1016/j.lithos.2006.03.057
https://openresearch-repository.anu.edu.au/bitstream/1885/17861/5/U8610899xPUB22006.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/17861/7/01_Kawakami_Sulfide_evolution_in_2006.pdf.jpg
Description
Summary:The high-temperature (HT) to ultrahigh-temperature (UHT) metamorphic rocks from Lützow-Holm Complex, East Antarctica show a systematic difference between sulfide assemblages in the rock matrix and those found as inclusions in the silicates stable in high

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