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2022
The Morelia-Acambay Fault System (MAFS) is located in the central western part of the Trans-Mexican Volcanic Belt (TMVB). The MAFS is a 30 km wide-transtensional shear zone made up of E-W and ENE-WSW oriented faults. Since middle Miocene (7-9 Ma), the seismotectonics of this fault system has controlled the evolution of E-W tectonic depressions (Zacapu,
Mennella L.[1] +6 more
openaire +1 more source
The Morelia-Acambay Fault System (MAFS) is located in the central western part of the Trans-Mexican Volcanic Belt (TMVB). The MAFS is a 30 km wide-transtensional shear zone made up of E-W and ENE-WSW oriented faults. Since middle Miocene (7-9 Ma), the seismotectonics of this fault system has controlled the evolution of E-W tectonic depressions (Zacapu,
Mennella L.[1] +6 more
openaire +1 more source
DETERMINACIÓN DE ESFUERZOS RESIDUALES EN UNIONES SOLDADAS DE PLACA DE ACERO INOXIDABLE
Dyna (Spain), 2015Mario Acosta Flores
exaly

