The Amorphous Component in Martian Basaltic Soil in Global Perspective from MSL and MER Missions
The mineralogy instrument CheMin onboard the MSL rover Curiosity analyzed by transmission XRD [1] the
Gespeichert in:
| Hauptverfasser: | , , , , , , , , , , , , , , , , , , , , , , , , |
|---|---|
| Format: | Tagungsbericht |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext bestellen |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | |
|---|---|
| container_issue | |
| container_start_page | |
| container_title | |
| container_volume | |
| creator | Morris, R. V. Ming, D. W. Blake, D. F. Vaniman, D. T. Bish, D. L. Chipera, S. J. Downs, R. T. Gellert, R. Treiman, A. H. Yen, A. S. Achilles, C. N. Anderson, R. C. Bristow, T. F. Crisp, J. A. Des Marais, D. J. Farmer, J. D. Grotzinger, J. P. Leshin, L. A. McAdam, A. C. Morookian, J. M. Morrison, S. M. Rampe, E. B. Sarrazin, P. C. Spanovich, N. Stolper, E. M. |
| description | The mineralogy instrument CheMin onboard the MSL rover Curiosity analyzed by transmission XRD [1] the |
| format | Conference Proceeding |
| fullrecord | <record><control><sourceid>nasa_CYI</sourceid><recordid>TN_cdi_nasa_ntrs_20130010069</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>20130010069</sourcerecordid><originalsourceid>FETCH-nasa_ntrs_201300100693</originalsourceid><addsrcrecordid>eNqFzLEKwjAQgOEuDqK-gcO9gJBaEBy1VB0MiO1ez5rSg-Su5KLPr4K70z988E-zWzM42AWJ4yBPhVLCKOw4ATFYjImQYY-KPlEHtZD_wtHLHT1cXNTRdYleDvooAWx9BuQH2OoKllRJWOfZpEevbvHrLFseqqY8rfhzbTlFbdcmL4zJjdlsiz_8BozKN44</addsrcrecordid><sourcetype>Publisher</sourcetype><iscdi>true</iscdi><recordtype>conference_proceeding</recordtype></control><display><type>conference_proceeding</type><title>The Amorphous Component in Martian Basaltic Soil in Global Perspective from MSL and MER Missions</title><source>NASA Technical Reports Server</source><creator>Morris, R. V. ; Ming, D. W. ; Blake, D. F. ; Vaniman, D. T. ; Bish, D. L. ; Chipera, S. J. ; Downs, R. T. ; Gellert, R. ; Treiman, A. H. ; Yen, A. S. ; Achilles, C. N. ; Anderson, R. C. ; Bristow, T. F. ; Crisp, J. A. ; Des Marais, D. J. ; Farmer, J. D. ; Grotzinger, J. P. ; Leshin, L. A. ; McAdam, A. C. ; Morookian, J. M. ; Morrison, S. M. ; Rampe, E. B. ; Sarrazin, P. C. ; Spanovich, N. ; Stolper, E. M.</creator><creatorcontrib>Morris, R. V. ; Ming, D. W. ; Blake, D. F. ; Vaniman, D. T. ; Bish, D. L. ; Chipera, S. J. ; Downs, R. T. ; Gellert, R. ; Treiman, A. H. ; Yen, A. S. ; Achilles, C. N. ; Anderson, R. C. ; Bristow, T. F. ; Crisp, J. A. ; Des Marais, D. J. ; Farmer, J. D. ; Grotzinger, J. P. ; Leshin, L. A. ; McAdam, A. C. ; Morookian, J. M. ; Morrison, S. M. ; Rampe, E. B. ; Sarrazin, P. C. ; Spanovich, N. ; Stolper, E. M.</creatorcontrib><description>The mineralogy instrument CheMin onboard the MSL rover Curiosity analyzed by transmission XRD [1] the <150 microns size fraction of putative global basaltic martian soil from scoops 4 and 5 of the Rocknest aeolian bedform (sol 81-120). Here, we combine chemical (APXS) and mineralogical (Mossbauer; MB) results from the MER rovers with chemical (APXS) and mineralogical (CheMin) results from Curiosity to constrain the relative proportions of amorphous and crystalline components, the bulk chemical composition of those components, and the</description><language>eng</language><publisher>Johnson Space Center</publisher><subject>Geophysics</subject><creationdate>2013</creationdate><rights>Copyright Determination: PUBLIC_USE_PERMITTED</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>309,780,800</link.rule.ids><linktorsrc>$$Uhttps://ntrs.nasa.gov/citations/20130010069$$EView_record_in_NASA$$FView_record_in_$$GNASA$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Morris, R. V.</creatorcontrib><creatorcontrib>Ming, D. W.</creatorcontrib><creatorcontrib>Blake, D. F.</creatorcontrib><creatorcontrib>Vaniman, D. T.</creatorcontrib><creatorcontrib>Bish, D. L.</creatorcontrib><creatorcontrib>Chipera, S. J.</creatorcontrib><creatorcontrib>Downs, R. T.</creatorcontrib><creatorcontrib>Gellert, R.</creatorcontrib><creatorcontrib>Treiman, A. H.</creatorcontrib><creatorcontrib>Yen, A. S.</creatorcontrib><creatorcontrib>Achilles, C. N.</creatorcontrib><creatorcontrib>Anderson, R. C.</creatorcontrib><creatorcontrib>Bristow, T. F.</creatorcontrib><creatorcontrib>Crisp, J. A.</creatorcontrib><creatorcontrib>Des Marais, D. J.</creatorcontrib><creatorcontrib>Farmer, J. D.</creatorcontrib><creatorcontrib>Grotzinger, J. P.</creatorcontrib><creatorcontrib>Leshin, L. A.</creatorcontrib><creatorcontrib>McAdam, A. C.</creatorcontrib><creatorcontrib>Morookian, J. M.</creatorcontrib><creatorcontrib>Morrison, S. M.</creatorcontrib><creatorcontrib>Rampe, E. B.</creatorcontrib><creatorcontrib>Sarrazin, P. C.</creatorcontrib><creatorcontrib>Spanovich, N.</creatorcontrib><creatorcontrib>Stolper, E. M.</creatorcontrib><title>The Amorphous Component in Martian Basaltic Soil in Global Perspective from MSL and MER Missions</title><description>The mineralogy instrument CheMin onboard the MSL rover Curiosity analyzed by transmission XRD [1] the <150 microns size fraction of putative global basaltic martian soil from scoops 4 and 5 of the Rocknest aeolian bedform (sol 81-120). Here, we combine chemical (APXS) and mineralogical (Mossbauer; MB) results from the MER rovers with chemical (APXS) and mineralogical (CheMin) results from Curiosity to constrain the relative proportions of amorphous and crystalline components, the bulk chemical composition of those components, and the</description><subject>Geophysics</subject><fulltext>true</fulltext><rsrctype>conference_proceeding</rsrctype><creationdate>2013</creationdate><recordtype>conference_proceeding</recordtype><sourceid>CYI</sourceid><recordid>eNqFzLEKwjAQgOEuDqK-gcO9gJBaEBy1VB0MiO1ez5rSg-Su5KLPr4K70z988E-zWzM42AWJ4yBPhVLCKOw4ATFYjImQYY-KPlEHtZD_wtHLHT1cXNTRdYleDvooAWx9BuQH2OoKllRJWOfZpEevbvHrLFseqqY8rfhzbTlFbdcmL4zJjdlsiz_8BozKN44</recordid><startdate>20130101</startdate><enddate>20130101</enddate><creator>Morris, R. V.</creator><creator>Ming, D. W.</creator><creator>Blake, D. F.</creator><creator>Vaniman, D. T.</creator><creator>Bish, D. L.</creator><creator>Chipera, S. J.</creator><creator>Downs, R. T.</creator><creator>Gellert, R.</creator><creator>Treiman, A. H.</creator><creator>Yen, A. S.</creator><creator>Achilles, C. N.</creator><creator>Anderson, R. C.</creator><creator>Bristow, T. F.</creator><creator>Crisp, J. A.</creator><creator>Des Marais, D. J.</creator><creator>Farmer, J. D.</creator><creator>Grotzinger, J. P.</creator><creator>Leshin, L. A.</creator><creator>McAdam, A. C.</creator><creator>Morookian, J. M.</creator><creator>Morrison, S. M.</creator><creator>Rampe, E. B.</creator><creator>Sarrazin, P. C.</creator><creator>Spanovich, N.</creator><creator>Stolper, E. M.</creator><scope>CYE</scope><scope>CYI</scope></search><sort><creationdate>20130101</creationdate><title>The Amorphous Component in Martian Basaltic Soil in Global Perspective from MSL and MER Missions</title><author>Morris, R. V. ; Ming, D. W. ; Blake, D. F. ; Vaniman, D. T. ; Bish, D. L. ; Chipera, S. J. ; Downs, R. T. ; Gellert, R. ; Treiman, A. H. ; Yen, A. S. ; Achilles, C. N. ; Anderson, R. C. ; Bristow, T. F. ; Crisp, J. A. ; Des Marais, D. J. ; Farmer, J. D. ; Grotzinger, J. P. ; Leshin, L. A. ; McAdam, A. C. ; Morookian, J. M. ; Morrison, S. M. ; Rampe, E. B. ; Sarrazin, P. C. ; Spanovich, N. ; Stolper, E. M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-nasa_ntrs_201300100693</frbrgroupid><rsrctype>conference_proceedings</rsrctype><prefilter>conference_proceedings</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Geophysics</topic><toplevel>online_resources</toplevel><creatorcontrib>Morris, R. V.</creatorcontrib><creatorcontrib>Ming, D. W.</creatorcontrib><creatorcontrib>Blake, D. F.</creatorcontrib><creatorcontrib>Vaniman, D. T.</creatorcontrib><creatorcontrib>Bish, D. L.</creatorcontrib><creatorcontrib>Chipera, S. J.</creatorcontrib><creatorcontrib>Downs, R. T.</creatorcontrib><creatorcontrib>Gellert, R.</creatorcontrib><creatorcontrib>Treiman, A. H.</creatorcontrib><creatorcontrib>Yen, A. S.</creatorcontrib><creatorcontrib>Achilles, C. N.</creatorcontrib><creatorcontrib>Anderson, R. C.</creatorcontrib><creatorcontrib>Bristow, T. F.</creatorcontrib><creatorcontrib>Crisp, J. A.</creatorcontrib><creatorcontrib>Des Marais, D. J.</creatorcontrib><creatorcontrib>Farmer, J. D.</creatorcontrib><creatorcontrib>Grotzinger, J. P.</creatorcontrib><creatorcontrib>Leshin, L. A.</creatorcontrib><creatorcontrib>McAdam, A. C.</creatorcontrib><creatorcontrib>Morookian, J. M.</creatorcontrib><creatorcontrib>Morrison, S. M.</creatorcontrib><creatorcontrib>Rampe, E. B.</creatorcontrib><creatorcontrib>Sarrazin, P. C.</creatorcontrib><creatorcontrib>Spanovich, N.</creatorcontrib><creatorcontrib>Stolper, E. M.</creatorcontrib><collection>NASA Scientific and Technical Information</collection><collection>NASA Technical Reports Server</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Morris, R. V.</au><au>Ming, D. W.</au><au>Blake, D. F.</au><au>Vaniman, D. T.</au><au>Bish, D. L.</au><au>Chipera, S. J.</au><au>Downs, R. T.</au><au>Gellert, R.</au><au>Treiman, A. H.</au><au>Yen, A. S.</au><au>Achilles, C. N.</au><au>Anderson, R. C.</au><au>Bristow, T. F.</au><au>Crisp, J. A.</au><au>Des Marais, D. J.</au><au>Farmer, J. D.</au><au>Grotzinger, J. P.</au><au>Leshin, L. A.</au><au>McAdam, A. C.</au><au>Morookian, J. M.</au><au>Morrison, S. M.</au><au>Rampe, E. B.</au><au>Sarrazin, P. C.</au><au>Spanovich, N.</au><au>Stolper, E. M.</au><format>book</format><genre>proceeding</genre><ristype>CONF</ristype><atitle>The Amorphous Component in Martian Basaltic Soil in Global Perspective from MSL and MER Missions</atitle><date>2013-01-01</date><risdate>2013</risdate><abstract>The mineralogy instrument CheMin onboard the MSL rover Curiosity analyzed by transmission XRD [1] the <150 microns size fraction of putative global basaltic martian soil from scoops 4 and 5 of the Rocknest aeolian bedform (sol 81-120). Here, we combine chemical (APXS) and mineralogical (Mossbauer; MB) results from the MER rovers with chemical (APXS) and mineralogical (CheMin) results from Curiosity to constrain the relative proportions of amorphous and crystalline components, the bulk chemical composition of those components, and the</abstract><cop>Johnson Space Center</cop><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext_linktorsrc |
| identifier | |
| ispartof | |
| issn | |
| language | eng |
| recordid | cdi_nasa_ntrs_20130010069 |
| source | NASA Technical Reports Server |
| subjects | Geophysics |
| title | The Amorphous Component in Martian Basaltic Soil in Global Perspective from MSL and MER Missions |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-25T20%3A54%3A56IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-nasa_CYI&rft_val_fmt=info:ofi/fmt:kev:mtx:book&rft.genre=proceeding&rft.atitle=The%20Amorphous%20Component%20in%20Martian%20Basaltic%20Soil%20in%20Global%20Perspective%20from%20MSL%20and%20MER%20Missions&rft.au=Morris,%20R.%20V.&rft.date=2013-01-01&rft_id=info:doi/&rft_dat=%3Cnasa_CYI%3E20130010069%3C/nasa_CYI%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true |