Sedimentological Signature of a Deformable Bed Preserved Beneath an Ice Stream in a Late Pleistocene Glacial Sequence, Ross Sea, Antarctica

Ellen A. Cowan; Poul Christoffersen; Ross D. Powell

doi:10.2110/jsr.2012.25

Sedimentological Signature of a Deformable Bed Preserved Beneath an Ice Stream in a Late Pleistocene Glacial Sequence, Ross Sea, Antarctica

Ellen A. Cowan
, Poul Christoffersen
, Ross D. Powell

Appalachian State University

Research output: Contribution to journal › Article › peer-review

Original language	American English
Journal	Journal of Sedimentary Research
Volume	82
DOIs	https://doi.org/10.2110/jsr.2012.25
State	Published - May 4 2012

Disciplines

Geology
Geomorphology

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10.2110/jsr.2012.25License: Unspecified

Cite this

@article{68fa5b1fcdcb48738b37e820a452fdc0,

title = "Sedimentological Signature of a Deformable Bed Preserved Beneath an Ice Stream in a Late Pleistocene Glacial Sequence, Ross Sea, Antarctica",

author = "Cowan, \{Ellen A.\} and Poul Christoffersen and Powell, \{Ross D.\}",

note = "Subglacial processes are described using a nested set of samples from AND-1B drill core collected from beneath the Ross Ice Shelf as part of the ANtarctic geologic DRILLing program (ANDRILL). An interval from the late Pleistocene was chosen for study because it is preserved in the sedimentary record, yet the depositional processes are applicable to the widely studied glacial conditions at the Last Glacial Maximum.",

year = "2012",

month = may,

day = "4",

doi = "10.2110/jsr.2012.25",

language = "American English",

volume = "82",

journal = "Journal of Sedimentary Research",

}

TY - JOUR

T1 - Sedimentological Signature of a Deformable Bed Preserved Beneath an Ice Stream in a Late Pleistocene Glacial Sequence, Ross Sea, Antarctica

AU - Cowan, Ellen A.

AU - Christoffersen, Poul

AU - Powell, Ross D.

N1 - Subglacial processes are described using a nested set of samples from AND-1B drill core collected from beneath the Ross Ice Shelf as part of the ANtarctic geologic DRILLing program (ANDRILL). An interval from the late Pleistocene was chosen for study because it is preserved in the sedimentary record, yet the depositional processes are applicable to the widely studied glacial conditions at the Last Glacial Maximum.

PY - 2012/5/4

Y1 - 2012/5/4

UR - http://archives.datapages.com/data/sepm/journals/082/082004/270_gsjsedres820270.htm

U2 - 10.2110/jsr.2012.25

DO - 10.2110/jsr.2012.25

M3 - Article

VL - 82

JO - Journal of Sedimentary Research

JF - Journal of Sedimentary Research

ER -