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New time-constraints on provenance, metamorphism and exhumation of the Bahía Mansa Metamorphic Complex on the Main Chiloé Island, south-central Chile
(Servicio Nacional de Geología y Minería (SERNAGEOMIN), 2008)
New time constraints for the age of metamorphism at the ancestral Pacific Gondwana margin of southern Chile (42-52°S)
(Servicio Nacional de Geología y Minería (SERNAGEOMIN), 2002)
Thermal metamorphism of mantle chromites and the stability of noble‑metal nanoparticles
(Springer, 2015)
The Loma Baya complex in south-western Mexico is a volume of chromitite-bearing oceanic mantle that records a complex metamorphic history, defined by a first stage of hydrous metamorphism overprinted by a short-lived thermal ...
Thermal metamorphism of mantle chromites and the stability of noble-metal nanoparticles
(2015)
The Loma Baya complex in south-western Mexico is a volume of chromitite-bearing oceanic mantle that records a complex metamorphic history, defined by a first stage of hydrous metamorphism overprinted by a short-lived thermal ...
P–T–time evolution of the Mejillones metamorphic complex: insights into late triassic to early jurassic orogenic processes in northern Chile
(Elsevier, 2017)
Better constrained pressure-temperature (P-T) histories of metamorphic complexes along the Andean continental
margin are important for understanding the late Paleozoic and Mesozoic tectonic evolution of the southwestern
margin ...
Tectono-metamorphic evolution of a convergent back-arc: The Famatinian orogen, Sierra de Quilmes, Sierras Pampeanas, NW Argentina
(Geological Society of America, 2017-06)
Back-arcs are hot regions of enduring weakness in the hinterland of subduction zones that are commonly sites of strain localization, forming mobile belts that, in some cases, develop into mountain belts. Their evolution ...