A west-to-east geologic transect across the Peninsular Ranges batholith, San Diego County, California: Zircon 176Hf/177Hf evidence for the mixing of crustal- and mantle-derived magmas, and comparisons with the Sierra Nevada batholith

Memoir of the Geological Society of America

Volumn 211, Issue , 2014, Pages 499-536

  Shaw, Stirling E ^a   Todd, Victoria R ^b   Kimbrough, David L ^c   Pearson, Norman J ^a  

^a MACQUARIE UNIVERSITY   (Australia)

^b Department of Geological Sciences San Diego State University ^*  (United States)

^c SAN DIEGO STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

GEOCHRONOLOGY; GRANITE; LEAD; MIXING; ZIRCON;

CHEMICAL BEHAVIOR; CRYSTALLIZATION AGE; EARLY CRETACEOUS; GRAVITY ANOMALIES; PALEOPROTEROZOIC; PENINSULAR RANGES BATHOLITH; SIERRA NEVADA BATHOLITH; TUOLUMNE INTRUSIVE SUITES;

HAFNIUM;

BATHOLITH; CRETACEOUS; EMPLACEMENT; HAFNIUM; I-TYPE ROCK; PLUTON; PROTEROZOIC; S-TYPE ROCK; SUTURE ZONE; ZIRCON;

CALIFORNIA; COAST RANGES; PENINSULAR RANGES; SAN DIEGO COUNTY; UNITED STATES;

EID: 84900525322     PISSN: 00721069     EISSN: None     Source Type: Book Series    
DOI: 10.1130/2014.1211(15)     Document Type: Article

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