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Activity

2024

• FIRST CYCLE OR POLYCYCLIC? COMBINING APATITE AND ZIRCON DETRITAL U-Pb GEOCHRONOLOGY AND GEOCHEMISTRY TO ASSESS SEDIMENT RECYCLING IN THE SOUTHWESTERN MONTANA FORELAND BASIN, NORTH AMERICAN CORDILLERA
  T71 The Changing Cordilleran Margin: Permian through Eocene Tectonism, Magmatism, and General Geology from Western Mexico through Northern California and Eastward
  Sunday, 22 September 2024

  1:30 PM - 5:30 PM

  304A

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2023

• CHRONOLOGICAL FRAMEWORK FOR THE LOWER CRETACEOUS SECTION IN SOUTHWESTERN MONTANA BASED ON DETRITAL ZIRCON U-PB GEOCHRONOLOGY FROM MULTIPLE LITHOLOGIES
  T20 Maximum Depositional Ages (MDAs) from Detrital Mineral Geochronology: Recent Advances in Sampling, Experimental Designs, Interpretive Tacts, and Chronostratigraphic Applications
  Sunday, 15 October 2023

  8:00 AM - 12:00 PM

  320

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2022

• KINEMATICS, TIMING, AND MAGNITUDE OF SHORTENING WITHIN THE CRETACEOUS SEVIER-LARAMIDE FOLD-THRUST BELT OF IDAHO AND MONTANA
  32 From the Sevier to Laramide: Connecting Hinterland to Foreland by Tectonics, Structure, and Sedimentation
  Thursday, 17 March 2022

  8:00 AM - 12:00 PM

  CBC-A 112

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2021

• MIDDLE ALBIAN PROVENANCE, SEDIMENT DISPERSAL, AND FORELAND BASIN DYNAMICS IN SOUTHWESTERN MONTANA, NORTH AMERICAN CORDILLERA
  T143 Insights into Cordilleran Tectonics and Magmatism from the Sedimentary Record
  Tuesday, 12 October 2021

  8:00 AM - 12:00 PM

  Portland Ballroom 255 (Hybrid Room)
• DETRITAL ZIRCON U-PB GEOCHRONOLOGY OF CRETACEOUS STRATA IN THE SOUTHWESTERN MONTANA FORELAND BASIN PROVIDES NEW TEMPORAL CONTROL FOR THE ONSET OF LARAMIDE DEFORMATION
  T143 Insights into Cordilleran Tectonics and Magmatism from the Sedimentary Record
  Tuesday, 12 October 2021

  8:00 AM - 12:00 PM

  Portland Ballroom 255 (Hybrid Room)

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2020

• DETRITAL ZIRCON PROVENANCE OF THE LOWER-UPPER CRETACEOUS BLACKLEAF FORMATION (UPPER INTERVALS) IN SOUTHWESTERN MONTANA, USA: IMPLICATIONS FOR REGIONAL TECTONICS AND SEDIMENTATION PATTERNS
  T199 Assembling Laurentia: Growth of the Western Continental Margin by Subduction, with or without Terrane Accretion, 190-70 Ma I
  Thursday, 29 October 2020

  1:30 PM - 5:30 PM

  Meeting Rooms