Mary K. Todt
Idaho State University, Pocatello, ID
Activity
2016
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THE LEMHI ARCH OF EAST-CENTRAL IDAHO: A STRANDED FAULT BLOCK WITHIN THE WESTERN LAURENTIAN RIFT MARGIN
18 Source to Sink, Proterozoic to Today: Erosion, Sediment Transport, and the Stratigraphic Record of Surface ProcessesThursday, 19 May 20168:00 AM - 12:00 PMCrest Room
2014
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SEDIMENTARY PROVENANCE OF THE UPPER CAMBRIAN WORM CREEK QUARTZITE, IDAHO, USING U-PB AND LU-HF ISOTOPIC ANALYSIS OF ZIRCON GRAINS
28 Precambrian II: Meso- and Neoproterozoic Evolution of Western Laurentia II: In Honor of Don WinstonWednesday, 21 May 20148:00 AM - 12:00 PMGaines Hall 101
2013
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SEDIMENTARY PROVENANCE OF THE UPPER CAMBRIAN WORM CREEK QUARTZITE, IDAHO, USING U-PB AND LU-HF ISOTOPIC ANALYSIS OF ZIRCON GRAINS
T56 The Life and Death of Mobile Belts along the North American Cordillera: Advances in Understanding the Long- Term Construction of Continental Margins (Posters)Sunday, 27 October 20139:00 AM - 6:30 PMHall D
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NEOPROTEROZOIC TO CAMBRIAN PASSIVE MARGIN? EVIDENCE FOR ACTIVE TECTONISM DURING THE SAUK TRANSGRESSION IN CENTRAL IDAHO AND MONTANA
T56 The Life and Death of Mobile Belts along the North American Cordillera: Advances in Understanding the Long- Term Construction of Continental Margins (Posters)Sunday, 27 October 20139:00 AM - 6:30 PMHall D