TY  - GEN 
AU  - Angiboust, Samuel
AU  - Cambeses Torres, Aitor
AU  - Hyppolito, Thais
AU  - Glodny, Johanes
AU  - Monié, Patrick
AU  - Calderón, Mauricio
AU  - Caetano, Juliani
PY  - 2018
UR  - https://hdl.handle.net/10481/101504
AB  - Diego de Almagro Island was formed by the subduction and accretion of several seafloor-derived tectonic slices with very heterogeneous ages and pressure-temperature-time (P-T-t) paths. The highest element of the pile (the Lazaro unit) evidences...
LA  - eng
TI  - A 100-m.y.-long window onto mass-flow processes in the Patagonian Mesozoic subduction zone (Diego de Almagro Island, Chile)
DO  - 10.1130/B31891.1
ER  -