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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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 |