Modeling the formation of Menrva impact crater on Titan: Implications for habitability
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F21%3A87022" target="_blank" >RIV/60460709:41330/21:87022 - isvavai.cz</a>
Výsledek na webu
<a href="https://www.sciencedirect.com/science/article/pii/S0019103521003365?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0019103521003365?via%3Dihub</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.icarus.2021.114679" target="_blank" >10.1016/j.icarus.2021.114679</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Modeling the formation of Menrva impact crater on Titan: Implications for habitability
Popis výsledku v původním jazyce
Titan is unique in the solar system: it is an ocean world, an icy world, an organic world, and has a dense atmosphere. It is a geologically active world as well, with ongoing exogenic processes, such as rainfall, sediment transportation and deposition, erosion, and possible endogenic processes, such as tectonism and cryovolcanism. This combination of an organic and an ocean world makes Titan a prime target for astrobiological research, as biosignatures may be present in its surface, in impact melt deposits and in cryovolcanic flows, as well as in deep ice and water ocean underneath the outer ice shell. Impact craters are important sites in this context, as they may have allowed an exchange of materials between Titans layers, in particular between the surface, composed of organic sediments over icy bedrock, and the subsurface ocean. It is also possible that impacts may have favored the advance of prebiotic chemical reactions themselves, by providing thermal energy that would allow these react
Název v anglickém jazyce
Modeling the formation of Menrva impact crater on Titan: Implications for habitability
Popis výsledku anglicky
Titan is unique in the solar system: it is an ocean world, an icy world, an organic world, and has a dense atmosphere. It is a geologically active world as well, with ongoing exogenic processes, such as rainfall, sediment transportation and deposition, erosion, and possible endogenic processes, such as tectonism and cryovolcanism. This combination of an organic and an ocean world makes Titan a prime target for astrobiological research, as biosignatures may be present in its surface, in impact melt deposits and in cryovolcanic flows, as well as in deep ice and water ocean underneath the outer ice shell. Impact craters are important sites in this context, as they may have allowed an exchange of materials between Titans layers, in particular between the surface, composed of organic sediments over icy bedrock, and the subsurface ocean. It is also possible that impacts may have favored the advance of prebiotic chemical reactions themselves, by providing thermal energy that would allow these react
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10308 - Astronomy (including astrophysics,space science)
Návaznosti výsledku
Projekt
<a href="/cs/project/GJ20-27624Y" target="_blank" >GJ20-27624Y: SyntetiCká a srovnávací Hydrologie zEmě, MArsu a TitAnu (SCHEMATA)</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2021
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
ICARUS
ISSN
0019-1035
e-ISSN
0019-1035
Svazek periodika
2021
Číslo periodika v rámci svazku
370
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
12
Strana od-do
1-12
Kód UT WoS článku
000701351400012
EID výsledku v databázi Scopus
2-s2.0-85114720082