Johnson, S.E.Fletcher, J MFanning, ChristopherVernon, R HPaterson, S RTate, M C2015-12-132015-12-130191-8141http://hdl.handle.net/1885/88647The 108 km2 San José pluton forms part of the Jurassic to Cretaceous Peninsular Ranges batholith of northern Baja California, México. The pluton was formed by three nested, southward-migrating intrusive pulses, and the internal contacts between them indKeywords: Plutons; Ductility; Earthquake effects; Rheology; Thermal effects; Uranium; Geology; deformation; emplacement; expansion; foliation; Mesozoic; pluton; structural analysis; tonalite; Mexico Foliation development; Geochronology; Pluton Emplacement; Submagmatic flow; Subsolidus flowStructure, emplacement and lateral expansion of the San José tonalite pluton, Peninsular Ranges batholith, Baja California, México200310.1016/S0191-8141(03)00015-42015-12-12