PSEUDOTACHYLITE FROM McINTYRE ISLAND, ENDERBYLAND, EAST ANTARCTICA : EVIDENCE FOR A RAPID CRYSTALLIZATION
Pseudotachylite from McIntyre Island in Enderby Land, East Antarctica, occurs in a breccia zone composed of black material with glassy luster and fragments of host pyroxene gneiss which has undergone ultra-high temperature metamorphism as a constituent of the Archean Napier Complex. Under the optica...
Main Authors: | , |
---|---|
Format: | Report |
Language: | English |
Published: |
National Institute of Polar Research
1996
|
Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2824 http://id.nii.ac.jp/1291/00002824/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2824&item_no=1&attribute_id=18&file_no=1 |