Luke P. Beranek
Idaho State Univ, Pocatello, ID
Activity
2005
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EASTWARD MIGRATION OF THE CONTINENTAL DIVIDE IN IDAHO TRACKED BY DETRITAL ZIRCONS IN MIDDLE MIOCENE TO RECENT (16 TO 0 MA) SEDIMENTS OF THE SNAKE RIVER PLAIN
37 Provenance and Tectonics: New Models and Recent AdvancesSunday, 1 May 20058:20 AM - 12:00 PM
2004
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DETRITAL ZIRCONS FROM MIOCENE TO RECENT SEDIMENTS OF THE WESTERN CORDILLERAN OROGEN: OREGON-IDAHO GRABEN AND SNAKE RIVER PLAIN, IDAHO
T236 Regional Geology of the Northern Rockies: A Session Honoring Betty SkippWednesday, 10 November 20041:30 PM - 5:30 PM
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GHOST NEOPROTEROZOIC (750-600 MA) DETRITAL ZIRCONS WITH NO KNOWN SOURCE: QUATERNARY FLUVIAL AND AEOLIAN SANDS, EASTERN SNAKE RIVER PLAIN, IDAHO
36 Proterozoic Geology of the Northwest U.S.: Basement and Tectonic Setting of the Belt Basin and Succeeding Windermere SupergroupWednesday, 5 May 20048:40 AM - 12:00 PM