Origin of Chlorobenzene Detected by the Curiosity Rover in Yellowknife Bay: Evidence for Martian Organics in the Sheepbed Mudstone
The Sample Analysis at Mars (SAM) instrument on the Curiosity rover is designed to determine the inventory of organic and inorganic volatiles thermally evolved from solid samples using a combination of evolved gas analysis (EGA), gas chromatography mass spectrometry (GCMS), and tunable laser spectro...
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ftnasantrs:oai:casi.ntrs.nasa.gov:20140011764 2023-05-15T18:45:42+02:00 Origin of Chlorobenzene Detected by the Curiosity Rover in Yellowknife Bay: Evidence for Martian Organics in the Sheepbed Mudstone Brunner, A. Conrad, P. Ming, D. Grotzinger, J. Navarro-Gonzalez, R. Mahaffy, P. Glavin, D. Coll, P. Steele, A. Miller, K. Archer, D. Coscia, D. Freissnet, C. Martin, M. Summons, R. E. Buch, A. Sutter, B. Cabane, M. Eigenbrode, J. Szopa, C. Teinturier, S. Dworkin, J. McKay, C. Unclassified, Unlimited, Publicly available March 17, 2014 application/pdf http://hdl.handle.net/2060/20140011764 unknown Document ID: 20140011764 http://hdl.handle.net/2060/20140011764 Copyright, Distribution as joint owner in the copyright CASI Lunar and Planetary Science and Exploration JSC-CN-30543 Lunar and Planetary Science Conference; 17-21 Mar. 2014; The Woodlands, TX; United States 2014 ftnasantrs 2019-07-21T00:25:10Z The Sample Analysis at Mars (SAM) instrument on the Curiosity rover is designed to determine the inventory of organic and inorganic volatiles thermally evolved from solid samples using a combination of evolved gas analysis (EGA), gas chromatography mass spectrometry (GCMS), and tunable laser spectroscopy. Here we discuss the SAM EGA and GCMS measurements of volatiles released from the Sheepbed mudstone. We focus primarily on the elevated CBZ detections at CB and laboratory analog experiments conducted to help determine if CBZ is derived from primarily terrestrial, martian, or a combination of sources. Here we discuss the SAM EGA and GCMS measurements of volatiles released from the Sheepbed mudstone. We focus primarily on the elevated CBZ detections at CB and laboratory analog experiments conducted to help determine if CBZ is derived from primarily terrestrial, martian, or a combination of sources. Other/Unknown Material Yellowknife NASA Technical Reports Server (NTRS) Yellowknife Yellowknife Bay ENVELOPE(-114.336,-114.336,62.367,62.367) |
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 Brunner, A. Conrad, P. Ming, D. Grotzinger, J. Navarro-Gonzalez, R. Mahaffy, P. Glavin, D. Coll, P. Steele, A. Miller, K. Archer, D. Coscia, D. Freissnet, C. Martin, M. Summons, R. E. Buch, A. Sutter, B. Cabane, M. Eigenbrode, J. Szopa, C. Teinturier, S. Dworkin, J. McKay, C. Origin of Chlorobenzene Detected by the Curiosity Rover in Yellowknife Bay: Evidence for Martian Organics in the Sheepbed Mudstone |
topic_facet |
Lunar and Planetary Science and Exploration |
description |
The Sample Analysis at Mars (SAM) instrument on the Curiosity rover is designed to determine the inventory of organic and inorganic volatiles thermally evolved from solid samples using a combination of evolved gas analysis (EGA), gas chromatography mass spectrometry (GCMS), and tunable laser spectroscopy. Here we discuss the SAM EGA and GCMS measurements of volatiles released from the Sheepbed mudstone. We focus primarily on the elevated CBZ detections at CB and laboratory analog experiments conducted to help determine if CBZ is derived from primarily terrestrial, martian, or a combination of sources. Here we discuss the SAM EGA and GCMS measurements of volatiles released from the Sheepbed mudstone. We focus primarily on the elevated CBZ detections at CB and laboratory analog experiments conducted to help determine if CBZ is derived from primarily terrestrial, martian, or a combination of sources. |
format |
Other/Unknown Material |
author |
Brunner, A. Conrad, P. Ming, D. Grotzinger, J. Navarro-Gonzalez, R. Mahaffy, P. Glavin, D. Coll, P. Steele, A. Miller, K. Archer, D. Coscia, D. Freissnet, C. Martin, M. Summons, R. E. Buch, A. Sutter, B. Cabane, M. Eigenbrode, J. Szopa, C. Teinturier, S. Dworkin, J. McKay, C. |
author_facet |
Brunner, A. Conrad, P. Ming, D. Grotzinger, J. Navarro-Gonzalez, R. Mahaffy, P. Glavin, D. Coll, P. Steele, A. Miller, K. Archer, D. Coscia, D. Freissnet, C. Martin, M. Summons, R. E. Buch, A. Sutter, B. Cabane, M. Eigenbrode, J. Szopa, C. Teinturier, S. Dworkin, J. McKay, C. |
author_sort |
Brunner, A. |
title |
Origin of Chlorobenzene Detected by the Curiosity Rover in Yellowknife Bay: Evidence for Martian Organics in the Sheepbed Mudstone |
title_short |
Origin of Chlorobenzene Detected by the Curiosity Rover in Yellowknife Bay: Evidence for Martian Organics in the Sheepbed Mudstone |
title_full |
Origin of Chlorobenzene Detected by the Curiosity Rover in Yellowknife Bay: Evidence for Martian Organics in the Sheepbed Mudstone |
title_fullStr |
Origin of Chlorobenzene Detected by the Curiosity Rover in Yellowknife Bay: Evidence for Martian Organics in the Sheepbed Mudstone |
title_full_unstemmed |
Origin of Chlorobenzene Detected by the Curiosity Rover in Yellowknife Bay: Evidence for Martian Organics in the Sheepbed Mudstone |
title_sort |
origin of chlorobenzene detected by the curiosity rover in yellowknife bay: evidence for martian organics in the sheepbed mudstone |
publishDate |
2014 |
url |
http://hdl.handle.net/2060/20140011764 |
op_coverage |
Unclassified, Unlimited, Publicly available |
long_lat |
ENVELOPE(-114.336,-114.336,62.367,62.367) |
geographic |
Yellowknife Yellowknife Bay |
geographic_facet |
Yellowknife Yellowknife Bay |
genre |
Yellowknife |
genre_facet |
Yellowknife |
op_source |
CASI |
op_relation |
Document ID: 20140011764 http://hdl.handle.net/2060/20140011764 |
op_rights |
Copyright, Distribution as joint owner in the copyright |
_version_ |
1766236832795721728 |