MARS: RESPONSE OF ICE-RICH PERMAFROST TO MILANKOVITCH FORCING AND THE ORIGIN OF THE

high northern latitudes of Mars and verified the presence of shallow subsurface water ice. This subsurface ice, discovered by the Gamma Ray and Neutron Spectrometer Suite poleward of about 55 ◦ latitude on both hemispheres [1, 2, 3], represents

Bibliographic Details
Main Author: Introduction The Phoenix L
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Ice
permafrost
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.192.6867
http://www.lpi.usra.edu/meetings/lpsc2009/pdf/1429.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.192.6867 2023-05-15T16:36:44+02:00 MARS: RESPONSE OF ICE-RICH PERMAFROST TO MILANKOVITCH FORCING AND THE ORIGIN OF THE Introduction The Phoenix L The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.192.6867 http://www.lpi.usra.edu/meetings/lpsc2009/pdf/1429.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.192.6867 http://www.lpi.usra.edu/meetings/lpsc2009/pdf/1429.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.lpi.usra.edu/meetings/lpsc2009/pdf/1429.pdf text ftciteseerx 2016-01-07T16:57:16Z high northern latitudes of Mars and verified the presence of shallow subsurface water ice. This subsurface ice, discovered by the Gamma Ray and Neutron Spectrometer Suite poleward of about 55 ◦ latitude on both hemispheres [1, 2, 3], represents Text Ice permafrost Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description high northern latitudes of Mars and verified the presence of shallow subsurface water ice. This subsurface ice, discovered by the Gamma Ray and Neutron Spectrometer Suite poleward of about 55 ◦ latitude on both hemispheres [1, 2, 3], represents
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Introduction The Phoenix L
spellingShingle Introduction The Phoenix L
MARS: RESPONSE OF ICE-RICH PERMAFROST TO MILANKOVITCH FORCING AND THE ORIGIN OF THE
author_facet Introduction The Phoenix L
author_sort Introduction The Phoenix L
title MARS: RESPONSE OF ICE-RICH PERMAFROST TO MILANKOVITCH FORCING AND THE ORIGIN OF THE
title_short MARS: RESPONSE OF ICE-RICH PERMAFROST TO MILANKOVITCH FORCING AND THE ORIGIN OF THE
title_full MARS: RESPONSE OF ICE-RICH PERMAFROST TO MILANKOVITCH FORCING AND THE ORIGIN OF THE
title_fullStr MARS: RESPONSE OF ICE-RICH PERMAFROST TO MILANKOVITCH FORCING AND THE ORIGIN OF THE
title_full_unstemmed MARS: RESPONSE OF ICE-RICH PERMAFROST TO MILANKOVITCH FORCING AND THE ORIGIN OF THE
title_sort mars: response of ice-rich permafrost to milankovitch forcing and the origin of the
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.192.6867
http://www.lpi.usra.edu/meetings/lpsc2009/pdf/1429.pdf
genre Ice
permafrost
genre_facet Ice
permafrost
op_source http://www.lpi.usra.edu/meetings/lpsc2009/pdf/1429.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.192.6867
http://www.lpi.usra.edu/meetings/lpsc2009/pdf/1429.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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