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...

Full description

Bibliographic Details
Main Authors: DeVincenzi, Donald L., Bishop, Janice L., Southard, R., Murad, E., Schiffman, P.
Format: Other/Unknown Material
Language:unknown
Published: 2001
Subjects:
Online Access:http://hdl.handle.net/2060/20010046975
id ftnasantrs:oai:casi.ntrs.nasa.gov:20010046975
record_format openpolar
spelling 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)
institution Open Polar
collection 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