OD-OI80 RELATIONSHIPS AND THE THERMAL HISTORY OF BASAL ICE NEAR THE MARGINS OF TWO GLACIERS IN

ABSTRACT. When plotted on a SD-SISO diagram, the isotope values of basal ice formed by refreezing of melt water beneath the cold-based margin of a corrie glacier lie on a straight line with a slope of 5.5. This freezing slope differs from a slope of 7.2 for the basal ice layer of the cold-based ice...

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Main Author: Lyngen North Norway
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Ice cap
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.430.6085
http://www.igsoc.org/journal/34/118/igs_journal_vol34_issue118_pg265-268.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.430.6085
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.430.6085 2023-05-15T16:38:11+02:00 OD-OI80 RELATIONSHIPS AND THE THERMAL HISTORY OF BASAL ICE NEAR THE MARGINS OF TWO GLACIERS IN Lyngen North Norway The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.430.6085 http://www.igsoc.org/journal/34/118/igs_journal_vol34_issue118_pg265-268.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.430.6085 http://www.igsoc.org/journal/34/118/igs_journal_vol34_issue118_pg265-268.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.igsoc.org/journal/34/118/igs_journal_vol34_issue118_pg265-268.pdf text ftciteseerx 2016-01-08T04:38:46Z ABSTRACT. When plotted on a SD-SISO diagram, the isotope values of basal ice formed by refreezing of melt water beneath the cold-based margin of a corrie glacier lie on a straight line with a slope of 5.5. This freezing slope differs from a slope of 7.2 for the basal ice layer of the cold-based ice cap, Balgesvarri, which has not undergone refreezing. The latter slope is similar to that of 7.7 for the local precipitation. Co-isotope measurements from the two glaciers support the associatIOn of subglacial debris entrainment with refreezing processes. Text Ice cap Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description ABSTRACT. When plotted on a SD-SISO diagram, the isotope values of basal ice formed by refreezing of melt water beneath the cold-based margin of a corrie glacier lie on a straight line with a slope of 5.5. This freezing slope differs from a slope of 7.2 for the basal ice layer of the cold-based ice cap, Balgesvarri, which has not undergone refreezing. The latter slope is similar to that of 7.7 for the local precipitation. Co-isotope measurements from the two glaciers support the associatIOn of subglacial debris entrainment with refreezing processes.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Lyngen North Norway
spellingShingle Lyngen North Norway
OD-OI80 RELATIONSHIPS AND THE THERMAL HISTORY OF BASAL ICE NEAR THE MARGINS OF TWO GLACIERS IN
author_facet Lyngen North Norway
author_sort Lyngen North Norway
title OD-OI80 RELATIONSHIPS AND THE THERMAL HISTORY OF BASAL ICE NEAR THE MARGINS OF TWO GLACIERS IN
title_short OD-OI80 RELATIONSHIPS AND THE THERMAL HISTORY OF BASAL ICE NEAR THE MARGINS OF TWO GLACIERS IN
title_full OD-OI80 RELATIONSHIPS AND THE THERMAL HISTORY OF BASAL ICE NEAR THE MARGINS OF TWO GLACIERS IN
title_fullStr OD-OI80 RELATIONSHIPS AND THE THERMAL HISTORY OF BASAL ICE NEAR THE MARGINS OF TWO GLACIERS IN
title_full_unstemmed OD-OI80 RELATIONSHIPS AND THE THERMAL HISTORY OF BASAL ICE NEAR THE MARGINS OF TWO GLACIERS IN
title_sort od-oi80 relationships and the thermal history of basal ice near the margins of two glaciers in
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.430.6085
http://www.igsoc.org/journal/34/118/igs_journal_vol34_issue118_pg265-268.pdf
genre Ice cap
genre_facet Ice cap
op_source http://www.igsoc.org/journal/34/118/igs_journal_vol34_issue118_pg265-268.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.430.6085
http://www.igsoc.org/journal/34/118/igs_journal_vol34_issue118_pg265-268.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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