ICE SHEET MODELING DURING HIGH-OBLIQUITY CLIMATES ON MARS: APPLICATION TO
Introduction: Deposits on the flanks of the large Tharsis Montes volcanoes have been recognized to be of glacial origin [1,2,3]. These Amazonian-aged deposits display three distinct facies, ridged, knobby, and smooth [4], each of which can be associated with different glacial processes [1]. We use t...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.174.6157 2023-05-15T16:40:20+02:00 ICE SHEET MODELING DURING HIGH-OBLIQUITY CLIMATES ON MARS: APPLICATION TO Tharsis Montes Tropical Mountain Glaciation J. L. Fastook D. E. Shean J. W. Head The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.174.6157 http://www.lpi.usra.edu/meetings/lpsc2006/pdf/1794.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.174.6157 http://www.lpi.usra.edu/meetings/lpsc2006/pdf/1794.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.lpi.usra.edu/meetings/lpsc2006/pdf/1794.pdf text ftciteseerx 2016-01-07T16:10:26Z Introduction: Deposits on the flanks of the large Tharsis Montes volcanoes have been recognized to be of glacial origin [1,2,3]. These Amazonian-aged deposits display three distinct facies, ridged, knobby, and smooth [4], each of which can be associated with different glacial processes [1]. We use the fundamental differences between the atmospheric Text Ice Sheet Unknown |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
Introduction: Deposits on the flanks of the large Tharsis Montes volcanoes have been recognized to be of glacial origin [1,2,3]. These Amazonian-aged deposits display three distinct facies, ridged, knobby, and smooth [4], each of which can be associated with different glacial processes [1]. We use the fundamental differences between the atmospheric |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Tharsis Montes Tropical Mountain Glaciation J. L. Fastook D. E. Shean J. W. Head |
spellingShingle |
Tharsis Montes Tropical Mountain Glaciation J. L. Fastook D. E. Shean J. W. Head ICE SHEET MODELING DURING HIGH-OBLIQUITY CLIMATES ON MARS: APPLICATION TO |
author_facet |
Tharsis Montes Tropical Mountain Glaciation J. L. Fastook D. E. Shean J. W. Head |
author_sort |
Tharsis Montes |
title |
ICE SHEET MODELING DURING HIGH-OBLIQUITY CLIMATES ON MARS: APPLICATION TO |
title_short |
ICE SHEET MODELING DURING HIGH-OBLIQUITY CLIMATES ON MARS: APPLICATION TO |
title_full |
ICE SHEET MODELING DURING HIGH-OBLIQUITY CLIMATES ON MARS: APPLICATION TO |
title_fullStr |
ICE SHEET MODELING DURING HIGH-OBLIQUITY CLIMATES ON MARS: APPLICATION TO |
title_full_unstemmed |
ICE SHEET MODELING DURING HIGH-OBLIQUITY CLIMATES ON MARS: APPLICATION TO |
title_sort |
ice sheet modeling during high-obliquity climates on mars: application to |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.174.6157 http://www.lpi.usra.edu/meetings/lpsc2006/pdf/1794.pdf |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
http://www.lpi.usra.edu/meetings/lpsc2006/pdf/1794.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.174.6157 http://www.lpi.usra.edu/meetings/lpsc2006/pdf/1794.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766030730297606144 |