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Resultats globals: 6 registres trobats en 0.02 segons.
Articles, 6 registres trobats
Articles 6 registres trobats  
1.
19 p, 4.6 MB Evidence of an oceanic impact and megatsunami sedimentation in Chryse Planitia, Mars / Rodriguez, J. Alexis P. (Planetary Science Institute) ; Robertson, Darrel K. (NASA Ames Research Center) ; Kargel, Jeffrey S. (Planetary Science Institute) ; Baker, Victor R. (University of Arizona) ; Berman, Daniel (Planetary Science Institute) ; Cohen, Jacob (NASA Ames Research Center) ; Costard, Francois (Université Paris-Saclay) ; Komatsu, Goro (Università D'Annunzio) ; Lopez, Anthony (Planetary Science Institute) ; Miyamoto, Hideaki (University of Tokyo) ; Zarroca Bonet, Mario (Universitat Autònoma de Barcelona. Departament de Geologia)
In 1976, NASA's Viking 1 Lander (V1L) was the first spacecraft to operate successfully on the Martian surface. The V1L landed near the terminus of an enormous catastrophic flood channel, Maja Valles. [...]
2022 - 10.1038/s41598-022-18082-2
Scientific reports, Vol. 12 (December 2022) , art. 19589  
Registre complet - Creative Commons
2.
12 p, 3.1 MB North polar trough formation due to in-situ erosion as a source of young ice in mid-latitudinal mantles on Mars / Rodriguez, J. Alexis P. (Planetary Science Institute) ; Tanaka, Kenneth L. (Planetary Science Institute) ; Bramson, Ali M. (Purdue University) ; Leonard, Gregory J. (University of Arizona) ; Baker, Victor R. (University of Arizona) ; Zarroca Bonet, Mario (Universitat Autònoma de Barcelona. Departament de Geologia)
The clockwise spiral of troughs marking the Martian north polar plateau forms one of the planet's youngest megastructures. One popular hypothesis posits that the spiral pattern resulted as troughs underwent poleward migration. [...]
2021 - 10.1038/s41598-021-83329-3
Scientific reports, Vol. 11 (March 2021) , art. 6750  
Registre complet - Creative Commons
3.
9 p, 2.8 MB Martian outflow channels : How did their source aquifers form, and why did they drain so rapidly? / Rodriguez, J. Alexis P. (NASA Ames Research Center) ; Kargel, Jeffrey S. (University of Arizona. Department of Hydrology & Water Resources) ; Baker, Victor R. (University of Arizona. Department of Hydrology & Water Resources) ; Gulick, Virginia C. (SETI Institute) ; Berman, Daniel (Planetary Science Institute) ; Fairén, Alberto G. (Cornell University. Department of Astronomy) ; Linares, Rogelio (Universitat Autònoma de Barcelona. Departament de Geologia) ; Zarroca Bonet, Mario (Universitat Autònoma de Barcelona. Departament de Geologia) ; Yan, Jianguo (Wuhan University. State Key Laboratory of Information Engineering in Surveying) ; Miyamoto, Hideaki (University of Tokyo) ; Glines, Natalie (SETI Institute)
Catastrophic floods generated ~3. 2 Ga by rapid groundwater evacuation scoured the Solar System's most voluminous channels, the southern circum-Chryse outflow channels. Based on Viking Orbiter data analysis, it was hypothesized that these outflows emanated from a global Hesperian cryosphere-confined aquifer that was infused by south polar meltwater infiltration into the planet's upper crust. [...]
2015 - 10.1038/srep13404
Scientific reports, Vol. 5 (September 2015) , art. 13404  
Registre complet - Creative Commons
4.
8 p, 2.1 MB Tsunami waves extensively resurfaced the shorelines of an early Martian ocean / Rodriguez, J. Alexis P. (NASA Ames Research Center) ; Fairén, Alberto G. (Cornell University. Department of Astronomy) ; Tanaka, Kenneth L. (United States Geological Survey) ; Zarroca Bonet, Mario (Universitat Autònoma de Barcelona. Departament de Geologia) ; Linares, Rogelio (Universitat Autònoma de Barcelona. Departament de Geologia) ; Platz, Thomas (Freie Universität Berlin. Planetary Sciences and Remote Sensing) ; Komatsu, Goro (Università d'Annunzio. International Research School of Planetary Sciences) ; Miyamoto, Hideaki (University of Tokyo. The University Museum) ; Kargel, Jeffrey S. (University of Arizona. Department of Hydrology & Water Resources) ; Yan, Jianguo (Wuhan University. State Key Laboratory of Information Engineering in Surveying, Mapping and Remote Sensing) ; Gulick, Virginia C (SETI Institute) ; Higuchi, Kana (Centro de Astrobiología (Madrid)) ; Baker, Victor R. (University of Arizona. Department of Hydrology & Water Resources) ; Glines, Natalie (SETI Institute)
It has been proposed that ~3. 4 billion years ago an ocean fed by enormous catastrophic floods covered most of the Martian northern lowlands. However, a persistent problem with this hypothesis is the lack of definitive paleoshoreline features. [...]
2016 - 10.1038/srep25106
Scientific reports, Vol. 6 (May 2016) , art. 25106  
Registre complet - Creative Commons
5.
14 p, 7.7 MB The Chaotic Terrains of Mercury Reveal a History of Planetary Volatile Retention and Loss in the Innermost Solar System / Rodriguez, J. Alexis P. (Planetary Science Institute (USA)) ; Leonard, Gregory J. (University of Arizona. Department of Planetary Sciences) ; Kargel, Jeffrey S. (Planetary Science Institute (USA)) ; Domingue, Deborah (Planetary Science Institute (USA)) ; Berman, Daniel (Planetary Science Institute (USA)) ; Banks, Maria (NASA Goddard Space Flight Center) ; Zarroca Bonet, Mario (Universitat Autònoma de Barcelona. Departament de Geologia) ; Linares, Rogelio (Universitat Autònoma de Barcelona. Departament de Geologia) ; Marchi, Simone (Southwest Research Institute (USA)) ; Baker, Victor R. (University of Arizona. Department of Hydrology and Atmospheric Sciences) ; Webster, Kevin D. (Planetary Science Institute (USA)) ; Sykes, Mark (Planetary Science Institute (USA))
Mercury's images obtained by the 1974 Mariner 10 flybys show extensive cratered landscapes degraded into vast knob fields, known as chaotic terrain (AKA hilly and lineated terrain). For nearly half a century, it was considered that these terrains formed due to catastrophic quakes and ejecta fallout produced by the antipodal Caloris basin impact. [...]
2020 - 10.1038/s41598-020-59885-5
Scientific reports, Vol. 10 (March 2020) , art. 4737  
Registre complet - Creative Commons
6.
9 p, 2.5 MB The 1997 Mars Pathfinder Spacecraft Landing Site : Spillover Deposits from an Early Mars Inland Sea / Rodriguez, J. A. P. (Planetary Science Institute) ; Baker, Victor R (University of Arizona. Department of Hydrology & Atmospheric Sciences) ; Liu, Tao (University of Arizona. Department of Hydrology & Atmospheric Sciences) ; Zarroca Bonet, Mario (Universitat Autònoma de Barcelona. Departament de Geologia) ; Travis, B. (Planetary Science Institute) ; Hui, T. (University of Arizona. Department of Hydrology & Atmospheric Sciences) ; Komatsu, Goro (Università D'Annunzio. International Research School of Planetary Sciences) ; Berman, Daniel (Planetary Science Institute) ; Linares, Rogelio (Universitat Autònoma de Barcelona. Departament de Geologia) ; Sykes, M. V. (Planetary Science Institute) ; Banks, Maria (NASA Goddard Space Flight Center) ; Kargel, J. S. (Planetary Science Institute)
The Martian outflow channels comprise some of the largest known channels in the Solar System. Remote-sensing investigations indicate that cataclysmic floods likely excavated the channels ~3. 4 Ga. Previous studies show that, in the southern circum-Chryse region, their flooding pathways include hundreds of kilometers of channel floors with upward gradients. [...]
2019 - 10.1038/s41598-019-39632-1
Scientific reports, Vol. 9, Núm. 1 (December 2019) , art. 4045  
Registre complet - Creative Commons

Vegeu també: autors amb noms similars
1 Baker, Victor R
5 Baker, Victor R.
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