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|b .M37 2021
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|a 559.923
|2 23
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| 245 |
0 |
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|a Mars geological enigmas :
|b from the late noachian epoch to the present day /
|c edited by Richard J. Soare [and more].
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| 260 |
|
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|a [S.l.] :
|b Elsevier,
|c 2021.
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| 300 |
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|a 1 online resource
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| 336 |
|
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|a text
|b txt
|2 rdacontent
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| 337 |
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|a computer
|b c
|2 rdamedia
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| 338 |
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|a online resource
|b cr
|2 rdacarrier
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|a <P>1. Current enigmas identified by the Curiosity rover at the Gale crater</p> <p><U><b>Node I </b></U><i><b>What sourced the enormous flows and volumes that formed the outflow channels and highland-margin contacts of ancient Mars? </b></i>2. The fluvial interpretation of outflow channels on Mars: landforms, processes and paleoenvironmental implications 3. Was there an early Mars ocean? 4. Dry megafloods on Mars: formation of the outflow channels by voluminous effusions of low viscosity lava</p> <p><U><b>Node II </b></U><i><b>Can impact craters be used to derive reliable surface ages on Mars? </b></i>5. Challenges in crater chronology arising from the Jezero impact crater 6. The role of secondary craters on Martian crater chronology</p> <p><U><b>Node III </b></U><i><b>The perplexing story of methane on Mars </b></i>7. Methane on Mars: subsurface sourcing and conflicting atmospheric measurements 8. A review of the meteor shower hypothesis for methane on Mars</p> <p><U><b>Node IV </b></U><i><b>Does water flow on Martian slopes? </b></i>9. The possible role of water in recent surface-processes on Mars 10. Dry formation of recent Martian slope-features</p> <p><U><b>Node V </b></U><i><b>Earth analogues for Mars -- a plethora of choice! </b></i>11. The McMurdo Dry Valleys of Antarctica: a geological, environmental and ecological analog to the Martian surfac 12. The Atacama Desert: a window into late Mars surface habitability 13. Ancient life in diverse habitats from the Pilbara Craton and Mount Bruce Supergroup, western Australia: analogues for early Mars?</p> <p><U><b>Node VI </b></U><i><b>The freeze-thaw cycling of water at/near the Martian surface: present, past and possible? </b></i>14. Pingo-like mounds and possible periglaciation/glaciation at/adjacent to the Moreux impact crater, Mars 15. Thermokarst-like depressions on Mars: age constraints on ice degradation in Utopia Planitia</p> <p><U><b>Node VII </b></U><i><b>Hemispheres together: towards understanding the Mars dichotomy </b></i>16. Forging the Mars crustal-dichotomy: the giant impact hypothesis 17. Endogenic origin of the Martian hemispheric dichotomy? <i>James Roberts</i></p>
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| 504 |
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|a Includes bibliographical references and index.
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| 651 |
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0 |
|a Mars (Planet)
|x Geology.
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| 650 |
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0 |
|a Geological mapping.
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| 651 |
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6 |
|a Mars (Plan�ete)
|x G�eologie.
|0 (CaQQLa)201-0077560
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| 650 |
|
6 |
|a Cartographie g�eologique.
|0 (CaQQLa)201-0009518
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| 650 |
|
7 |
|a Geological mapping
|2 fast
|0 (OCoLC)fst00940582
|
| 650 |
|
7 |
|a Planets
|x Geology
|2 fast
|0 (OCoLC)fst01065145
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| 651 |
|
7 |
|a Mars (Planet)
|2 fast
|0 (OCoLC)fst01243063
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| 700 |
1 |
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|a Soare, Richard J.
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| 776 |
0 |
8 |
|i Print version:
|z 9780128202463
|
| 776 |
0 |
8 |
|i Print version:
|z 0128202459
|z 9780128202456
|w (OCoLC)1225624595
|
| 856 |
4 |
0 |
|u https://sciencedirect.uam.elogim.com/science/book/9780128202456
|z Texto completo
|
