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PSEUDOTACHYLITE FROM McINTYRE ISLAND, ENDERBYLAND, EAST ANTARCTICA : EVIDENCE FOR A RAPID CRYSTALLIZATION
https://doi.org/10.15094/00002824
https://doi.org/10.15094/00002824a5c1b387-887b-4bdc-96f6-eeef2b23f1d6
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002409871 (1.2 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1996-09-01 | |||||
タイトル | ||||||
タイトル | PSEUDOTACHYLITE FROM McINTYRE ISLAND, ENDERBYLAND, EAST ANTARCTICA : EVIDENCE FOR A RAPID CRYSTALLIZATION | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | pseudotachylite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | McIntyre Island | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Enderby Land | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Antarctica | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | WDS-compositional mapping | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00002824 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
論文名よみ | ||||||
その他のタイトル | PSEUDOTACHYLITE FROM McINTYRE ISLAND, ENDERBYLAND, EAST ANTARCTICA : EVIDENCE FOR A RAPID CRYSTALLIZATION | |||||
著者名よみ |
モトヨシ, ヨウイチ
× モトヨシ, ヨウイチ |
|||||
著者名(英) |
MOTOYOSHI, Yoichi
× MOTOYOSHI, Yoichi |
|||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | 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 optical and electron microscopes, the rock in the zone demonstrates a distinct sheared texture with extremely fine-grained materials, a part of which may be a glass. Abundant euhedral garnets occur in the fine-grained part, and their chemical compositions are quite heterogeneous from domain to domain. In view of the evidence that no garnet was observed in the host pyroxene gneiss, these garnets are likely to have crystallized very rapidly in the melt or solidified melt. Because of the chemical heterogeneity of garnet in the pseudotachylite even in a small domain, it is highly difficult to estimate the P-T conditions by means of geothermobarometric techniques using the mineral chemistries of microlites. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1072335X | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences 巻 9, p. 65-75, 発行日 1996-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |