| タイトル | Accretionary origin for the late Archean Ashuanipi Complex of Canada |
| 本文（外部サイト） | http://hdl.handle.net/2060/19890012866 |
| 著者（英） | Percival, J. A. |
| 著者所属（英） | Geological Survey of Canada |
| 発行日 | 1988-01-01 |
| 言語 | eng |
| 内容記述 | The Ashuanipi complex is one of the largest massif granulite terrains of the Canadian Shield. It makes up the eastern end of the 2000 km long, lower-grade, east-west belts of the Archean Superior Province, permitting lithological, age and tectonic correlation. Numerous lithological, geochemical and metamorphic similarities to south Indian granulites suggest common processes and invite comparison of tectonic evolution. The Ashuanipi granulite terrain of the Cannadian Superior Province was studied in detail, and an origin through self-melting of a 55 km thick accretionary wedge seems possible. |
| NASA分類 | GEOPHYSICS |
| レポートNO | 89N22237 |
| 権利 | No Copyright |
| URI | https://repository.exst.jaxa.jp/dspace/handle/a-is/142286 |
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