High temperatures and inverted metamorphism in the schist of Sierra de Salinas, California

Earth and Planetary Science Letters

Volumn 241, Issue 3-4, 2006, Pages 422-437

  Kidder, Steven ^a,b   Ducea, Mihai N ^a  

^a University of Arizona   (United States)

^b CALIFORNIA INSTITUTE OF TECHNOLOGY   (United States)

Author keywords

Accretion; Pelona schist; POR schists; Salinia; Schist of Sierra de Salinas; Shear heating; Subduction

Indexed keywords

ACCRETION; BRITTLE FAULT; PLUTONIC ROCKS; ROCK DEFORMATION; SCHISTS; SHEAR HEATING; SUBDUCTION;

DEFORMATION; FELDSPAR; GARNETS; GRANITE; GRANULAR MATERIALS; HEAT CONDUCTION; HIGH TEMPERATURE EFFECTS; MATHEMATICAL MODELS; PETROLOGY; SEDIMENTS; SHEAR STRESS;

METAMORPHIC ROCKS;

GEOBAROMETRY; METAMORPHISM; SCHIST;

CALIFORNIA; NORTH AMERICA; SALINAS VALLEY; UNITED STATES;

EID: 30744464897     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2005.11.037     Document Type: Article

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