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
Main Authors: Kawakami, Tetsuo, Ellis, David, Christy, Andrew
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2015
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
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

Similar Items