The Pliocene Lost River found to west: Detrital zircon evidence of drainage disruption along a subsiding hotspot track

Journal of Volcanology and Geothermal Research

Volumn 188, Issue 1-3, 2009, Pages 237-249

  Hodges, Mary K V ^a   Link, Paul Karl ^b   Fanning, C Mark ^c  

^a U S GEOLOGICAL SURVEY   (United States)

^b IDAHO STATE UNIVERSITY   (United States)

^c AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

Axial Volcanic Zone; Big Lost River; Cryogenian magmatism; detrital zircon; drainage disruption; Idaho; INL; Neogene; Snake River Plain

Indexed keywords

AXIAL VOLCANIC ZONE; DETRITAL ZIRCON; MAGMATISMS; NEO GENES; SNAKE RIVER PLAINS; VOLCANIC ZONE;

AQUIFERS; CATCHMENTS; CORE DRILLING; CORE SAMPLES; DRAINAGE; DRILLS; GEOCHRONOLOGY; SAND; SILICATE MINERALS; TECTONICS; VOLCANOES; ZIRCON;

RIVERS;

DETRITAL DEPOSIT; DRAINAGE; GEOCHRONOLOGY; HOT SPOT; MAGMATISM; NEOGENE; PALEOHYDROLOGY; PROTEROZOIC; PROVENANCE; SHRIMP DATING; URANIUM-LEAD DATING; ZIRCON;

BIG LOST RIVER; IDAHO; NORTH AMERICA; SNAKE RIVER PLAIN; UNITED STATES;

EID: 71749098338     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2009.08.019     Document Type: Article

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