The Mammoth Peak sheeted complex, Tuolumne batholith, Sierra Nevada, California: A record of initial growth or late thermal contraction in a magma chamber?

Contributions to Mineralogy and Petrology

Volumn 158, Issue 4, 2009, Pages 447-470

  Žák, Jiřá ^a,b   Paterson, Scott R ^c   Janoušek, Vojtěch ^a,b   Kabele, Petr ^d  

^a CHARLES UNIVERSITY   (Czech Republic)

^b CZECH GEOLOGICAL SURVEY   (Czech Republic)

^c UNIVERSITY OF SOUTHERN CALIFORNIA   (United States)

^d CZECH TECHNICAL UNIVERSITY IN PRAGUE   (Czech Republic)

Author keywords

Emplacement; Granite; Incremental growth; Magma chamber; Pluton; Thermal mechanical modeling

Indexed keywords

BATHOLITH; CONTRACTION; CRACK PROPAGATION; DIKE; EMPLACEMENT; FINITE ELEMENT METHOD; GRANODIORITE; GROWTH RATE; LAYERED INTRUSION; MAGMA CHAMBER; MAGMATISM; MELTING; NUMERICAL MODEL; PLUTON;

CALIFORNIA; MAMMOTH MOUNTAIN; NORTH AMERICA; SIERRA NEVADA [CALIFORNIA]; UNITED STATES;

EID: 69849098720     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-009-0391-8     Document Type: Article

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