Reassessing classic evidence for warm-based Cryogenian ice on the western Laurentian margin: The “striated pavement” of the Mineral Fork Formation, USA

  • T. M. Vandyk
  • , C. Kettler
  • , B. J. Davies
  • , G. A. Shields
  • , I. Candy
  • , D. P. Le Heron

Publications: Contribution to journalArticlePeer Reviewed

Original languageEnglish
Article number106345
Number of pages18
JournalPrecambrian Research
Volume363
DOIs
Publication statusPublished - Sept 2021

Funding

TMV gratefully acknowledges funding from the Postgraduate Research Grant of the International Association of Sedimentologists, the Postgraduate Research Grant of the British Society for Geomorphology and the Student Research Grant of the Society for Sedimentary Geology (SEPM). This work was supported by the Natural Environment Research Council [grant number NE/L002485/1]. We are most grateful for the constructive review of this manuscript and its previous iteration by 3 anonymous reviewers, Marie Busfield, Nicholas Eyles and Maarten Krabbendam.

Austrian Fields of Science 2012

  • 105101 General geology

Keywords

  • Cryogenian
  • Geomorphology
  • Glaciation
  • Snowball Earth
  • BIG COTTONWOOD FORMATION
  • NEOPROTEROZOIC GLACIATION
  • NORTHERN UTAH
  • EDIACARAN GLACIATION
  • RECORD
  • SNOWBALL EARTH
  • POCATELLO FORMATION
  • UINTA MOUNTAIN-GROUP
  • GLACIGENIC DEBRIS FLOWS
  • WASATCH MOUNTAINS

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