Resumen
The Coast Ranges of southern Chile are underlain for the most part by a variably metamorphosed subduction complex of late Paleozoic age. In a contribution to IGCP 279, "Terranes in Latin America,' the author reviews the depositional and metamorphic development of this huge accretionary unit developed in the Gondwana continental margin. South to north transport of the accreted material parallel to the continental margin may prove to have been an important tectonic process in the region. -Journal summary
| Idioma original | Inglés |
|---|---|
| Páginas (desde-hasta) | 183-188 |
| Número de páginas | 6 |
| Publicación | Episodes |
| Volumen | 11 |
| N.º | 3 |
| Estado | Publicada - 1988 |
Áreas temáticas de ASJC Scopus
- Ciencias planetarias y de la Tierra (miscelánea)
- Ciencias planetarias y de la Tierra (todo)
Huella Profundice en los temas de investigación de 'Late Paleozoic subduction and accretion in southern Chile'. En conjunto forman una huella única.
Citar esto
Herve, F. (1988). Late Paleozoic subduction and accretion in southern Chile. Episodes, 11(3), 183-188.