Large-volume, low-δ18O rhyolites of the central Snake River Plain, Idaho, USA

Geology

Volumn 33, Issue 10, 2005, Pages 821-824

  Boroughs, Scott ^a   Wolff, John ^a   Bonnichsen, Bill ^b   Godchaux, Martha ^b   Larson, Peter ^a  

^a WASHINGTON STATE UNIVERSITY   (United States)

^b Idaho Geological Survey   (United States)

Author keywords

Meteoric hydrothermal alteration; Oxygen isotopes; Rhyolites; Snake River Plain

Indexed keywords

METEORIC-HYDROTHERMAL ALTERATION; OXYGEN ISOTOPES; RHYOLITES;

FELDSPAR; GEOCHEMISTRY; ISOTOPES; OXYGEN; TRACE ELEMENTS;

VOLCANIC ROCKS;

IGNEOUS GEOCHEMISTRY; LAVA; OXYGEN ISOTOPE; PETROGENESIS; RHYOLITE; TUFF;

IDAHO; NORTH AMERICA; SNAKE RIVER PLAIN; UNITED STATES; WESTERN HEMISPHERE; WORLD;

EID: 26844547879     PISSN: 00917613     EISSN: 00917613     Source Type: Journal    
DOI: 10.1130/G21723.1     Document Type: Article

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