Mineral abundances at the final four curiosity study sites and implications for their formation
• We derive the modal mineralogy of the four MSL landing site candidates. • The largest abundance of phyllosilicates (30–70vol%) is found in Mawrth Vallis. • The Holden deposit composition suggests transport and deposition of altered basalts. • The Eberswalde mineralogy consists of detrital clays an...
Ausführliche Beschreibung
Autor*in: |
Poulet, F. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2014 |
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Schlagwörter: |
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Umfang: |
12 |
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Übergeordnetes Werk: |
Enthalten in: Development of electrophysiological and behavioural measures of electrode discrimination in adult cochlear implant users - Mathew, Rajeev ELSEVIER, 2018, international journal of solar system studies, Orlando, Fla |
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Übergeordnetes Werk: |
volume:231 ; year:2014 ; day:1 ; month:03 ; pages:65-76 ; extent:12 |
Links: |
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DOI / URN: |
10.1016/j.icarus.2013.11.023 |
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ELV023082844 |
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• We derive the modal mineralogy of the four MSL landing site candidates. • The largest abundance of phyllosilicates (30–70vol%) is found in Mawrth Vallis. • The Holden deposit composition suggests transport and deposition of altered basalts. • The Eberswalde mineralogy consists of detrital clays and authigenic phases. • At Gale, the low abundance of clays do not favor a complex and long drainage system. |
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• We derive the modal mineralogy of the four MSL landing site candidates. • The largest abundance of phyllosilicates (30–70vol%) is found in Mawrth Vallis. • The Holden deposit composition suggests transport and deposition of altered basalts. • The Eberswalde mineralogy consists of detrital clays and authigenic phases. • At Gale, the low abundance of clays do not favor a complex and long drainage system. |
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• We derive the modal mineralogy of the four MSL landing site candidates. • The largest abundance of phyllosilicates (30–70vol%) is found in Mawrth Vallis. • The Holden deposit composition suggests transport and deposition of altered basalts. • The Eberswalde mineralogy consists of detrital clays and authigenic phases. • At Gale, the low abundance of clays do not favor a complex and long drainage system. |
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