Differential Movement across Byrd Glacier, Antarctica, as indicated by Apatite (U–Th)/He thermochronology and geomorphological analysis

The objectives of this study were to assess possible differential movement across an inferred fault beneath Byrd Glacier, and to measure the timing of unroofing in this portion of the Transantarctic Mountains. Apatites separated from rock samples collected from known elevations at various locations...

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Bibliographic Details
Main Authors: D. J. Foley, E. Stump, M. Van Soest, K. X. Whipple, K. V. Hodges
Format: Text
Language:unknown
Published: Geological Society of London 2016
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Online Access:https://dx.doi.org/10.6084/m9.figshare.3453494
https://geolsoc.figshare.com/articles/journal_contribution/Differential_Movement_across_Byrd_Glacier_Antarctica_as_indicated_by_Apatite_U_Th_He_thermochronology_and_geomorphological___analysis/3453494