Supereruptions of the Snake River Plain: Two-stage derivation of low-δ18O rhyolites from normal-δ18O crust as constrained by Archean xenoliths

Geology

Volumn 38, Issue 6, 2010, Pages 503-506

  Watts, Kathryn E ^a   Leeman, William P ^b   Bindeman, Ilya N ^a   Larson, Peter B ^c  

^a UNIVERSITY OF OREGON   (United States)

^b USA   (United States)

^c WASHINGTON STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ARCHEAN; CRUSTAL XENOLITHS; DATA SUPPORT; ENDMEMBERS; HYDROTHERMALLY; ISOTOPE DEPLETION; ISOTOPIC MIXING; MAGMA GENESIS; MANTLE SOURCE; MIXING LINES; PARTIAL MELTING; PB ISOTOPES; RHYOLITIC; SNAKE RIVER PLAINS; TWO STAGE; VOLCANIC FIELD; YELLOWSTONES;

ISOTOPES; LEAD; NEODYMIUM; RIVERS; SEDIMENTARY ROCKS; STRONTIUM; VOLCANOES;

GRANITE;

CALDERA; EXPLOSIVE VOLCANISM; IGNEOUS GEOCHEMISTRY; ISOTOPIC COMPOSITION; LARGE IGNEOUS PROVINCE; MAGMA CHEMISTRY; MAGMATISM; MANTLE SOURCE; OXYGEN ISOTOPE; PARTIAL MELTING; RHYOLITE; VOLCANIC ERUPTION;

IDAHO; SNAKE RIVER PLAIN; UNITED STATES; YELLOWSTONE VOLCANIC PLATEAU;

EID: 77955954235     PISSN: 00917613     EISSN: 00917613     Source Type: Journal    
DOI: 10.1130/G30735.1     Document Type: Article

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