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Ophiolite Emplacement and the Effects of the Subduction of the Active Chile Ridge System: Heterogeneous Paleostress Regimes Recorded in the Taitao Ophiolite (Southern Chile)

The repeated north and southward migration of the Chile Triple junction, offshore the Península de Taitao, is expected to have imposed contrasting stress fields in the forearc for the last 6 Ma because of changes in convergence direction and rate of subducting plates. NNW-SSE to E-W and minor NE-SW...

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Publicado en:Andean Geology
Autores principales: Eugenio E. Veloso, Ryo Anma, Atsushi Yamaji
Formato: Artigo
Lenguaje:Inglês
Publicado: Servicio Nacional de Geología y Minería 2009
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Acceso en línea:https://www.redalyc.org/articulo.oa?id=173914379002
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