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
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Elsevier
2015
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/17861 |
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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