A5067399546- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- Geological and Geophysical Studies
- earthquake and tectonic studies
- Paleontology and Stratigraphy of Fossils
- Environmental and Cultural Studies in Latin America and Beyond
- Geological and Tectonic Studies in Latin America
University of Chile
2014-2023
Universidad del Desarrollo
2022
Universidad de Oviedo
2022
Universidad Andrés Bello
2021
Late Paleozoic to early Mesozoic subduction complexes formed during the evolution of southwestern Gondwana and extensively crop out along Chilean continental margin. Recent findings in northern Patagonia (40°–43°S) revealed that accretionary processes were active since Devonian when enhanced lithosphere stretching forearc led formation Chaitenia island arc. The extension crust consecutively developed a backarc basin, which culminated compressive episode re-amalgamated arc with This produced...
During the late Carboniferous–middle Permian, basement of Chilean Coastal Cordillera was deformed by Gondwanan Orogeny, developed subduction Paleo-Pacific plate under Gondwana from early Carboniferous. In Maule sector (35.4°S), following metamorphic rock units are distinguished: (i) Western Series, formed metapelites, metabasites, metacherts, metaconglomerates, and marbles, mixed in a channel, with probably ages between Cambrian Carboniferous; (ii) Eastern consisting metasediments fore-arc...