Iceland as a Model for Chemical Alteration on Mars
Subglacial volcanic activity on Iceland has led to the formation of a variety of silicate and iron oxide-rich alteration products that may serve as a model for chemical alteration on Mars. Multiple palagonitic tuffs, altered pillow lavas, hydrothermal springs and alteration at glacial run-off stream...
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ftnasantrs:oai:casi.ntrs.nasa.gov:20010046975 2023-05-15T16:44:05+02:00 Iceland as a Model for Chemical Alteration on Mars DeVincenzi, Donald L. Bishop, Janice L. Southard, R. Murad, E. Schiffman, P. Unclassified, Unlimited, Publicly available Jan. 18, 2001 application/pdf http://hdl.handle.net/2060/20010046975 unknown Document ID: 20010046975 http://hdl.handle.net/2060/20010046975 No Copyright CASI Lunar and Planetary Science and Exploration Lunar and Planetary Science Conference; 11-16 Mar. 2001; Houston, TX; United States 2001 ftnasantrs 2019-07-21T02:46:57Z Subglacial volcanic activity on Iceland has led to the formation of a variety of silicate and iron oxide-rich alteration products that may serve as a model for chemical alteration on Mars. Multiple palagonitic tuffs, altered pillow lavas, hydrothermal springs and alteration at glacial run-off streams were observed during a recent field trip in Iceland. Formation of alteration products and ferrihydrite in similar environments on Mars may have contributed to the ferric oxide-rich surface material there. The spectral and chemical properties of Icelandic alteration products and ferrihydrites are presented here. Other/Unknown Material Iceland NASA Technical Reports Server (NTRS) |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
Lunar and Planetary Science and Exploration |
spellingShingle |
Lunar and Planetary Science and Exploration DeVincenzi, Donald L. Bishop, Janice L. Southard, R. Murad, E. Schiffman, P. Iceland as a Model for Chemical Alteration on Mars |
topic_facet |
Lunar and Planetary Science and Exploration |
description |
Subglacial volcanic activity on Iceland has led to the formation of a variety of silicate and iron oxide-rich alteration products that may serve as a model for chemical alteration on Mars. Multiple palagonitic tuffs, altered pillow lavas, hydrothermal springs and alteration at glacial run-off streams were observed during a recent field trip in Iceland. Formation of alteration products and ferrihydrite in similar environments on Mars may have contributed to the ferric oxide-rich surface material there. The spectral and chemical properties of Icelandic alteration products and ferrihydrites are presented here. |
format |
Other/Unknown Material |
author |
DeVincenzi, Donald L. Bishop, Janice L. Southard, R. Murad, E. Schiffman, P. |
author_facet |
DeVincenzi, Donald L. Bishop, Janice L. Southard, R. Murad, E. Schiffman, P. |
author_sort |
DeVincenzi, Donald L. |
title |
Iceland as a Model for Chemical Alteration on Mars |
title_short |
Iceland as a Model for Chemical Alteration on Mars |
title_full |
Iceland as a Model for Chemical Alteration on Mars |
title_fullStr |
Iceland as a Model for Chemical Alteration on Mars |
title_full_unstemmed |
Iceland as a Model for Chemical Alteration on Mars |
title_sort |
iceland as a model for chemical alteration on mars |
publishDate |
2001 |
url |
http://hdl.handle.net/2060/20010046975 |
op_coverage |
Unclassified, Unlimited, Publicly available |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
CASI |
op_relation |
Document ID: 20010046975 http://hdl.handle.net/2060/20010046975 |
op_rights |
No Copyright |
_version_ |
1766034394052558848 |