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Mostrando ítems 1-10 de 13
The low‑grade basement at Península La Carmela, Chilean Patagonia: new data for unraveling the pre‑Permian basin nature of the Eastern Andean Metamorphic Complex
(2021)
The Eastern Andean Metamorphic Complex at Península La Carmela (48°50’S) consists of quartz-rich metaturbiditic sequences with tectonic slices of pillow metabasalt bodies deformed under low-grade metamorphic conditions. ...
The low-grade basement at Península La Carmela, Chilean Patagonia: new data for unraveling the pre-Permian basin nature of the Eastern Andean Metamorphic Complex
(Springer, 2021-07)
The Eastern Andean Metamorphic Complex at Península La Carmela (48°50’S) consists of quartz-rich metaturbiditic sequences with tectonic slices of pillow metabasalt bodies deformed under low-grade metamorphic conditions. ...
Geological and Structural Analisys of the Sunsás Belt in the Nova Brasilândia region Southeastern Rondonia StateAnálise Geológico-Estrutural do Cinturão Sunsás na Região de Nova Brasilândia - Sudeste de Rondônia
(Instituto de Geociências /Universidade Federal do Rio Grande do Sul, 2000)
Geodynamics of Late Carboniferous-Early Permian forearc in north Chile (28 degrees 30 '-29 degrees 30 ' S)
(2016)
A large section of the Late Palaeozoic forearc is exposed along the coastal ranges of north-central Chile (28 degrees-29 degrees 30'S). This is characterized by three lithotectonic units: (1) the Punta de Choros Metamorphic ...
Geotectônica e evolução crustal das faixas Rio Preto e Riacho do Pontal, estados da Bahia, Pernambuco e Piauí
(Universidade Federal de Minas GeraisUFMG, 2013-10-25)
The Rio Preto and Riacho do Pontal fold belts are part of the extensive Brasiliano / Pan- African branch of orogens of West Gondwana in Northeast Brazil, extending up to 600 km in a SWNE trend within the northwest and north ...