Late Paleozoic subduction and accretion in southern Chile

F. Herve

doi:10.18814/epiiugs/1988/v11i3/005

Late Paleozoic subduction and accretion in southern Chile

F. Herve

Facultad Ingeniería

Resultado de la investigación: Contribución a una revista › Artículo › revisión exhaustiva

138 Citas (Scopus)

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
DOI	https://doi.org/10.18814/epiiugs/1988/v11i3/005
Estado	Publicada - 1988

Áreas temáticas de ASJC Scopus

Ciencias planetarias y de la Tierra (todo)

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10.18814/epiiugs/1988/v11i3/005

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title = "Late Paleozoic subduction and accretion in southern Chile",

abstract = "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",

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AB - 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

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Late Paleozoic subduction and accretion in southern Chile

Resumen

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