Compact Reconnaissance Imaging Spectrometer for Mars
confirm many previous models and shed new light on the nature of polar surface materials, particularly in intermediate-albedo units of the polar layered deposits, many of which are found to be ice-rich. We identify hydrated non ice materials present in many low-albedo troughs, as well as in the circ...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.655.1406 2023-05-15T16:37:11+02:00 Compact Reconnaissance Imaging Spectrometer for Mars The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.655.1406 http://planetary.brown.edu/pdfs/3960.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.655.1406 http://planetary.brown.edu/pdfs/3960.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://planetary.brown.edu/pdfs/3960.pdf text ftciteseerx 2016-01-08T16:34:26Z confirm many previous models and shed new light on the nature of polar surface materials, particularly in intermediate-albedo units of the polar layered deposits, many of which are found to be ice-rich. We identify hydrated non ice materials present in many low-albedo troughs, as well as in the circumpolar erg that was previously associated with gypsum. We identify icy outlier deposits that may be related to subsurface thermophysical properties and permafrost. New observations of the gypsum-rich dune material constrain models for its formation and distribution. Intrinsic properties of ice content and grain size are found to be independent of the albedo of fine layered units and may provide a novel method for stratigraphic identification and correlation. Text Ice permafrost Unknown |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
confirm many previous models and shed new light on the nature of polar surface materials, particularly in intermediate-albedo units of the polar layered deposits, many of which are found to be ice-rich. We identify hydrated non ice materials present in many low-albedo troughs, as well as in the circumpolar erg that was previously associated with gypsum. We identify icy outlier deposits that may be related to subsurface thermophysical properties and permafrost. New observations of the gypsum-rich dune material constrain models for its formation and distribution. Intrinsic properties of ice content and grain size are found to be independent of the albedo of fine layered units and may provide a novel method for stratigraphic identification and correlation. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
Compact Reconnaissance Imaging Spectrometer for Mars |
spellingShingle |
Compact Reconnaissance Imaging Spectrometer for Mars |
title_short |
Compact Reconnaissance Imaging Spectrometer for Mars |
title_full |
Compact Reconnaissance Imaging Spectrometer for Mars |
title_fullStr |
Compact Reconnaissance Imaging Spectrometer for Mars |
title_full_unstemmed |
Compact Reconnaissance Imaging Spectrometer for Mars |
title_sort |
compact reconnaissance imaging spectrometer for mars |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.655.1406 http://planetary.brown.edu/pdfs/3960.pdf |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
http://planetary.brown.edu/pdfs/3960.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.655.1406 http://planetary.brown.edu/pdfs/3960.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766027484884631552 |