Search

Your search keyword '"Le Deit, Laetitia"' showing total 15 results
Start Over Author "Le Deit, Laetitia" Publication Type Electronic Resources
15 results on '"Le Deit, Laetitia"'

1. Radiation-induced alteration of apatite on the surface of Mars:first in situ observations with SuperCam Raman onboard Perseverance

Author

Clavé, E., Beyssac, O., Bernard, S., Royer, C., Lopez-Reyes, G., Schröder, S., Rammelkamp, K., Forni, O., Fau, A., Cousin, A., Manrique, J. A., Ollila, A., Madariaga, J. M., Aramendia, J., Sharma, S. K., Fornaro, T., Maurice, S., Wiens, R. C., Acosta-Maeda, Tayro, Agard, Christophe, Alberquilla, Fernando, Alvarez Llamas, Cesar, Anderson, Ryan, Applin, Daniel, Aramendia, Julene, Arana, Gorka, Beal, Roberta, Beck, Pierre, Bedford, Candice, Benzerara, Karim, Bernard, Sylvain, Bernardi, Pernelle, Bertrand, Tanguy, Beyssac, Olivier, Bloch, Thierry, Bonnet, Jean-Yves, Bousquet, Bruno, Boustelitane, Abderrahmane, Bouyssou Mann, Magali, Brand, Matthew, Cais, Philippe, Caravaca, Gwenael, De Pinedo, Kepa Castro Ortiz, Cazalla, Charlene, Charpentier, Antoine, Chide, Baptiste, Clavé, Elise, Clegg, Samuel, Cloutis, Ed, Coloma, Leire, Comellas, Jade, Connell, Stephanie, Cousin, Agnes, DeFlores, Lauren, Dehouck, Erwin, Delapp, Dot, Perez, Tomas Delgado, Deron, Robin, Donny, Christophe, Doressoundiram, Alain, Dromart, Gilles, Essunfeld, Ari, Fabre, Cecile, Fau, Amaury, Fischer, Woodward, Follic, Hugo, Forni, Olivier, Fouchet, Thierry, Francis, Raymond, Frydenvang, Jens, Gabriel, Travis, Gallegos, Zachary, García-Florentino, Cristina, Gasda, Patrick, Gasnault, Olivier, Gibbons, Erin, Gillier, Martin, Gomez, Laura, Gonzalez, Sofia, Grotzinger, John, Huidobro, Jennifer, Jacob, Xavier, Johnson, Jeffrey, Kalucha, Hemani, Kelly, Evan, Knutsen, Elise, Lacombe, Gaetan, Lamarque, Florentin, Lanza, Nina, Larmat, Carene, Laserna, Javier, Lasue, Jeremie, Le Deit, Laetitia, Le Mouelic, Stephane, Legett, Chip, Leveille, Richard, Lewin, Eric, Little, Cynthia, Loche, Mattéo, Lopez Reyes, Guillermo, Lorenz, Ralph, Lorigny, Eric, Madariaga, Juan Manuel, Madsen, Morten, Mandon, Lucia, Manelski, Henry, Mangold, Nicolas, Martinez, Jose Manrique, Martin, Noah, Martinez Frias, Jesus, Maurice, Sylvestre, Mcconnochie, Timothy, McLennan, Scott, Melikechi, Noureddine, Meslin, Pierre Yves, Meunier, Frederique, Mimoun, David, Montagnac, Gilles, Montmessin, Franck, Moros, Javier, Mousset, Valerie, Murdoch, Naomi, Nelson, Tony, Newell, Ray, Nicolas, Cécile, Newsom, Horton, O’Shea, Colleen, Ollila, Ann, Pantalacci, Philippe, Parmentier, Jonathan, Peret, Laurent, Perrachon, Pascal, Pilleri, Paolo, Pilorget, Cédric, Pinet, Patrick, Poblacion, Iratxe, Poulet, Francois, Quantin Nataf, Cathy, Rapin, William, Reyes, Ivan, Rigaud, Laurent, Robinson, Scott, Rochas, Ludovic, Root, Margaret, Ropert, Eloise, Rouverand, Léa, Royer, Clement, Perez, Fernando Rull, Said, David, Sans-Jofre, Pierre, Schroeder, Susanne, Seel, Fabian, Sharma, Shiv, Sheridan, Amanda, Sobron Sanchez, Pablo, Stcherbinine, Aurélien, Stott, Alex, Toplis, Michael, Turenne, Nathalie, Veneranda, Marco, Venhaus, Dawn, Wiens, Roger, Wolf, Uriah, Zastrow, Allison, Clavé, E., Beyssac, O., Bernard, S., Royer, C., Lopez-Reyes, G., Schröder, S., Rammelkamp, K., Forni, O., Fau, A., Cousin, A., Manrique, J. A., Ollila, A., Madariaga, J. M., Aramendia, J., Sharma, S. K., Fornaro, T., Maurice, S., Wiens, R. C., Acosta-Maeda, Tayro, Agard, Christophe, Alberquilla, Fernando, Alvarez Llamas, Cesar, Anderson, Ryan, Applin, Daniel, Aramendia, Julene, Arana, Gorka, Beal, Roberta, Beck, Pierre, Bedford, Candice, Benzerara, Karim, Bernard, Sylvain, Bernardi, Pernelle, Bertrand, Tanguy, Beyssac, Olivier, Bloch, Thierry, Bonnet, Jean-Yves, Bousquet, Bruno, Boustelitane, Abderrahmane, Bouyssou Mann, Magali, Brand, Matthew, Cais, Philippe, Caravaca, Gwenael, De Pinedo, Kepa Castro Ortiz, Cazalla, Charlene, Charpentier, Antoine, Chide, Baptiste, Clavé, Elise, Clegg, Samuel, Cloutis, Ed, Coloma, Leire, Comellas, Jade, Connell, Stephanie, Cousin, Agnes, DeFlores, Lauren, Dehouck, Erwin, Delapp, Dot, Perez, Tomas Delgado, Deron, Robin, Donny, Christophe, Doressoundiram, Alain, Dromart, Gilles, Essunfeld, Ari, Fabre, Cecile, Fau, Amaury, Fischer, Woodward, Follic, Hugo, Forni, Olivier, Fouchet, Thierry, Francis, Raymond, Frydenvang, Jens, Gabriel, Travis, Gallegos, Zachary, García-Florentino, Cristina, Gasda, Patrick, Gasnault, Olivier, Gibbons, Erin, Gillier, Martin, Gomez, Laura, Gonzalez, Sofia, Grotzinger, John, Huidobro, Jennifer, Jacob, Xavier, Johnson, Jeffrey, Kalucha, Hemani, Kelly, Evan, Knutsen, Elise, Lacombe, Gaetan, Lamarque, Florentin, Lanza, Nina, Larmat, Carene, Laserna, Javier, Lasue, Jeremie, Le Deit, Laetitia, Le Mouelic, Stephane, Legett, Chip, Leveille, Richard, Lewin, Eric, Little, Cynthia, Loche, Mattéo, Lopez Reyes, Guillermo, Lorenz, Ralph, Lorigny, Eric, Madariaga, Juan Manuel, Madsen, Morten, Mandon, Lucia, Manelski, Henry, Mangold, Nicolas, Martinez, Jose Manrique, Martin, Noah, Martinez Frias, Jesus, Maurice, Sylvestre, Mcconnochie, Timothy, McLennan, Scott, Melikechi, Noureddine, Meslin, Pierre Yves, Meunier, Frederique, Mimoun, David, Montagnac, Gilles, Montmessin, Franck, Moros, Javier, Mousset, Valerie, Murdoch, Naomi, Nelson, Tony, Newell, Ray, Nicolas, Cécile, Newsom, Horton, O’Shea, Colleen, Ollila, Ann, Pantalacci, Philippe, Parmentier, Jonathan, Peret, Laurent, Perrachon, Pascal, Pilleri, Paolo, Pilorget, Cédric, Pinet, Patrick, Poblacion, Iratxe, Poulet, Francois, Quantin Nataf, Cathy, Rapin, William, Reyes, Ivan, Rigaud, Laurent, Robinson, Scott, Rochas, Ludovic, Root, Margaret, Ropert, Eloise, Rouverand, Léa, Royer, Clement, Perez, Fernando Rull, Said, David, Sans-Jofre, Pierre, Schroeder, Susanne, Seel, Fabian, Sharma, Shiv, Sheridan, Amanda, Sobron Sanchez, Pablo, Stcherbinine, Aurélien, Stott, Alex, Toplis, Michael, Turenne, Nathalie, Veneranda, Marco, Venhaus, Dawn, Wiens, Roger, Wolf, Uriah, and Zastrow, Allison

Abstract

Planetary exploration relies considerably on mineral characterization to advance our understanding of the solar system, the planets and their evolution. Thus, we must understand past and present processes that can alter materials exposed on the surface, affecting space mission data. Here, we analyze the first dataset monitoring the evolution of a known mineral target in situ on the Martian surface, brought there as a SuperCam calibration target onboard the Perseverance rover. We used Raman spectroscopy to monitor the crystalline state of a synthetic apatite sample over the first 950 Martian days (sols) of the Mars2020 mission. We note significant variations in the Raman spectra acquired on this target, specifically a decrease in the relative contribution of the Raman signal to the total signal. These observations are consistent with the results of a UV-irradiation test performed in the laboratory under conditions mimicking ambient Martian conditions. We conclude that the observed evolution reflects an alteration of the material, specifically the creation of electronic defects, due to its exposure to the Martian environment and, in particular, UV irradiation. This ongoing process of alteration of the Martian surface needs to be taken into account for mineralogical space mission data analysis.

Published
2024

4. Amazonian-aged fluvial system and associated ice-related features in Terra Cimmeria, Mars

Author

Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, Jaumann, Ralf, Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, and Jaumann, Ralf

Abstract

The Martian climate throughout the Amazonian is widely believed to have been cold and hyper-arid, very similar to the current conditions. However, ubiquitous evidence of aqueous and glacial activity has been recently reported, including channels that can be tens to hundreds of kilometres long, alluvial and fluvial deposits, ice-rich mantles, and glacial and periglacial landforms. Here we study a ~340. km-long fluvial system located in the Terra Cimmeria region, in the southern mid-latitudes of Mars. The fluvial system is composed of an upstream catchment system with narrow glaciofluvial valleys and remnants of ice-rich deposits. We observe depositional features including fan-shaped deposits, and erosional features such as scour marks and streamlined islands. At the downstream section of this fluvial system is an outflow channel named Kārūn Valles, which displays a unique braided alluvial fan and terminates on the floor of the Ariadnes Colles basin. Our observations point to surface runoff of ice/snow melt as the water source for this fluvial activity. According to our crater size-frequency distribution analysis the entire fluvial system formed during early to middle Amazonian, between ~1.8-0.2+0.2Ga to 510-40+40Ma. Hydraulic modelling indicates that the Kārūn Valles and consequently the alluvial fan formation took place in geologically short-term event(s). We conclude that liquid water was present in Terra Cimmeria during the early to middle Amazonian, and that Mars during that time may have undergone several episodic glacial-related events.

Published
2016

5. Mineralogy, provenance, and diagenesis of a potassic basaltic sandstone on Mars: CheMin X-ray diffraction of the Windjana sample (Kimberley area, Gale Crater).

Author

Treiman, Allan H, Treiman, Allan H, Bish, David L, Vaniman, David T, Chipera, Steve J, Blake, David F, Ming, Doug W, Morris, Richard V, Bristow, Thomas F, Morrison, Shaunna M, Baker, Michael B, Rampe, Elizabeth B, Downs, Robert T, Filiberto, Justin, Glazner, Allen F, Gellert, Ralf, Thompson, Lucy M, Schmidt, Mariek E, Le Deit, Laetitia, Wiens, Roger C, McAdam, Amy C, Achilles, Cherie N, Edgett, Kenneth S, Farmer, Jack D, Fendrich, Kim V, Grotzinger, John P, Gupta, Sanjeev, Morookian, John Michael, Newcombe, Megan E, Rice, Melissa S, Spray, John G, Stolper, Edward M, Sumner, Dawn Y, Vasavada, Ashwin R, Yen, Albert S, Treiman, Allan H, Treiman, Allan H, Bish, David L, Vaniman, David T, Chipera, Steve J, Blake, David F, Ming, Doug W, Morris, Richard V, Bristow, Thomas F, Morrison, Shaunna M, Baker, Michael B, Rampe, Elizabeth B, Downs, Robert T, Filiberto, Justin, Glazner, Allen F, Gellert, Ralf, Thompson, Lucy M, Schmidt, Mariek E, Le Deit, Laetitia, Wiens, Roger C, McAdam, Amy C, Achilles, Cherie N, Edgett, Kenneth S, Farmer, Jack D, Fendrich, Kim V, Grotzinger, John P, Gupta, Sanjeev, Morookian, John Michael, Newcombe, Megan E, Rice, Melissa S, Spray, John G, Stolper, Edward M, Sumner, Dawn Y, Vasavada, Ashwin R, and Yen, Albert S

Abstract

The Windjana drill sample, a sandstone of the Dillinger member (Kimberley formation, Gale Crater, Mars), was analyzed by CheMin X-ray diffraction (XRD) in the MSL Curiosity rover. From Rietveld refinements of its XRD pattern, Windjana contains the following: sanidine (21% weight, ~Or95); augite (20%); magnetite (12%); pigeonite; olivine; plagioclase; amorphous and smectitic material (~25%); and percent levels of others including ilmenite, fluorapatite, and bassanite. From mass balance on the Alpha Proton X-ray Spectrometer (APXS) chemical analysis, the amorphous material is Fe rich with nearly no other cations-like ferrihydrite. The Windjana sample shows little alteration and was likely cemented by its magnetite and ferrihydrite. From ChemCam Laser-Induced Breakdown Spectrometer (LIBS) chemical analyses, Windjana is representative of the Dillinger and Mount Remarkable members of the Kimberley formation. LIBS data suggest that the Kimberley sediments include at least three chemical components. The most K-rich targets have 5.6% K2O, ~1.8 times that of Windjana, implying a sediment component with >40% sanidine, e.g., a trachyte. A second component is rich in mafic minerals, with little feldspar (like a shergottite). A third component is richer in plagioclase and in Na2O, and is likely to be basaltic. The K-rich sediment component is consistent with APXS and ChemCam observations of K-rich rocks elsewhere in Gale Crater. The source of this sediment component was likely volcanic. The presence of sediment from many igneous sources, in concert with Curiosity's identifications of other igneous materials (e.g., mugearite), implies that the northern rim of Gale Crater exposes a diverse igneous complex, at least as diverse as that found in similar-age terranes on Earth.

Published
2016

6. Amazonian-aged fluvial system and associated ice-related features in Terra Cimmeria, Mars

Author

Universiteit Utrecht, Coastal dynamics, Fluvial systems and Global change, Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, Jaumann, Ralf, Universiteit Utrecht, Coastal dynamics, Fluvial systems and Global change, Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, and Jaumann, Ralf

Published
2016

7. Mineralogy, provenance, and diagenesis of a potassic basaltic sandstone on Mars: CheMin X-ray diffraction of the Windjana sample (Kimberley area, Gale Crater).

Author

Treiman, Allan H, Treiman, Allan H, Bish, David L, Vaniman, David T, Chipera, Steve J, Blake, David F, Ming, Doug W, Morris, Richard V, Bristow, Thomas F, Morrison, Shaunna M, Baker, Michael B, Rampe, Elizabeth B, Downs, Robert T, Filiberto, Justin, Glazner, Allen F, Gellert, Ralf, Thompson, Lucy M, Schmidt, Mariek E, Le Deit, Laetitia, Wiens, Roger C, McAdam, Amy C, Achilles, Cherie N, Edgett, Kenneth S, Farmer, Jack D, Fendrich, Kim V, Grotzinger, John P, Gupta, Sanjeev, Morookian, John Michael, Newcombe, Megan E, Rice, Melissa S, Spray, John G, Stolper, Edward M, Sumner, Dawn Y, Vasavada, Ashwin R, Yen, Albert S, Treiman, Allan H, Treiman, Allan H, Bish, David L, Vaniman, David T, Chipera, Steve J, Blake, David F, Ming, Doug W, Morris, Richard V, Bristow, Thomas F, Morrison, Shaunna M, Baker, Michael B, Rampe, Elizabeth B, Downs, Robert T, Filiberto, Justin, Glazner, Allen F, Gellert, Ralf, Thompson, Lucy M, Schmidt, Mariek E, Le Deit, Laetitia, Wiens, Roger C, McAdam, Amy C, Achilles, Cherie N, Edgett, Kenneth S, Farmer, Jack D, Fendrich, Kim V, Grotzinger, John P, Gupta, Sanjeev, Morookian, John Michael, Newcombe, Megan E, Rice, Melissa S, Spray, John G, Stolper, Edward M, Sumner, Dawn Y, Vasavada, Ashwin R, and Yen, Albert S

Abstract

The Windjana drill sample, a sandstone of the Dillinger member (Kimberley formation, Gale Crater, Mars), was analyzed by CheMin X-ray diffraction (XRD) in the MSL Curiosity rover. From Rietveld refinements of its XRD pattern, Windjana contains the following: sanidine (21% weight, ~Or95); augite (20%); magnetite (12%); pigeonite; olivine; plagioclase; amorphous and smectitic material (~25%); and percent levels of others including ilmenite, fluorapatite, and bassanite. From mass balance on the Alpha Proton X-ray Spectrometer (APXS) chemical analysis, the amorphous material is Fe rich with nearly no other cations-like ferrihydrite. The Windjana sample shows little alteration and was likely cemented by its magnetite and ferrihydrite. From ChemCam Laser-Induced Breakdown Spectrometer (LIBS) chemical analyses, Windjana is representative of the Dillinger and Mount Remarkable members of the Kimberley formation. LIBS data suggest that the Kimberley sediments include at least three chemical components. The most K-rich targets have 5.6% K2O, ~1.8 times that of Windjana, implying a sediment component with >40% sanidine, e.g., a trachyte. A second component is rich in mafic minerals, with little feldspar (like a shergottite). A third component is richer in plagioclase and in Na2O, and is likely to be basaltic. The K-rich sediment component is consistent with APXS and ChemCam observations of K-rich rocks elsewhere in Gale Crater. The source of this sediment component was likely volcanic. The presence of sediment from many igneous sources, in concert with Curiosity's identifications of other igneous materials (e.g., mugearite), implies that the northern rim of Gale Crater exposes a diverse igneous complex, at least as diverse as that found in similar-age terranes on Earth.

Published
2016

8. Amazonian-aged fluvial system and associated ice-related features in Terra Cimmeria, Mars

Author

Universiteit Utrecht, Coastal dynamics, Fluvial systems and Global change, Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, Jaumann, Ralf, Universiteit Utrecht, Coastal dynamics, Fluvial systems and Global change, Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, and Jaumann, Ralf

Published
2016

9. Amazonian-aged fluvial system and associated ice-related features in Terra Cimmeria, Mars

Author

Universiteit Utrecht, Coastal dynamics, Fluvial systems and Global change, Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, Jaumann, Ralf, Universiteit Utrecht, Coastal dynamics, Fluvial systems and Global change, Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, and Jaumann, Ralf

Published
2016

10. Origin and significance of decameter-scale polygons in the lower Peace Vallis fan of Gale crater, Mars

Author

Johnson Space Center, NASA Astrobiology Institute (US), Centre National D'Etudes Spatiales (France), California Institute of Technology, European Research Council, Oehler, Dorothy Z., Mangold, Nicolas, Hallet, Bernat, Fairén, Alberto G., Le Deit, Laetitia, Williams, Amy J., Sletten, Ronald S., Martínez-Frías, J., Johnson Space Center, NASA Astrobiology Institute (US), Centre National D'Etudes Spatiales (France), California Institute of Technology, European Research Council, Oehler, Dorothy Z., Mangold, Nicolas, Hallet, Bernat, Fairén, Alberto G., Le Deit, Laetitia, Williams, Amy J., Sletten, Ronald S., and Martínez-Frías, J.

Abstract

Decameter-scale polygons are extensively developed in the Bedded Fractured (BF) Unit of the lower Peace Vallis fan. The polygons occur in a likely extension of the Gillespie Lake Member, north of Yellowknife Bay, the section first drilled by the Mars Science Laboratory (MSL) mission. We examine hypotheses for the origin of these polygons to provide insight into the history of Gale crater. The polygons are ∼4–30 m across, square to rectangular, and defined by ∼0.5–4 m wide, generally straight troughs with orthogonal intersections. Polygon networks are typically oriented-orthogonal systems, with occasional nearly circular patterns, hundreds of meters across. Potential origins include cooling of lava, and for sedimentary units, syneresis, unloading, weathering, desiccation, impact processes, and cold-climate thermal contraction. Cold-climate thermal contraction is the hypothesis most consistent with the sedimentary nature of the BF Unit and the polygon morphology, geometry, networks, and apparent restriction to the coarse-grained Gillespie Lake Member. A periglacial setting further provides the best analogs for the circular networks and is consistent with geologic context and MSL data. Most of the decametric polygons appear to be ancient. They are confined to the Hesperian BF Unit, and only a few of their bounding fractures extend into younger or recently exposed units. In this regard, they differ from the majority of proposed thermal-contraction polygons on Mars, as those are generally thought to be young features, and, accordingly, the history of formation, preservation and reactivation of the decametric polygons is likely to be more complex than that of any proposed young polygons on Mars. The decametric polygons in the BF Unit may represent landforms developed in a cold but still comparatively wet interlude between a clement early Mars and the much drier and colder planet of today.

Published
2016

11. The high-resolution map of Oxia Planum, Mars; the landing site of the ExoMars Rosalind Franklin rover mission

Author

Fawdon, Peter, Orgel, Csilla, Adeli, Solmaz, Balme, Matt, Calef, Fred J., Davis, Joel M., Frigeri, Alessandro, Grindrod, Peter, Hauber, Ernst, Le Deit, Laetitia, Loizeau, Damien, Nass, Andrea, Quantin-Nataf, Cathy, Sefton-Nash, Elliot, Thomas, Nick, Torres, Ines, Vago, Jorge L., Volat, Matthieu, De Witte, Sander, Altieri, Francesca, Apuzzo, Andrea, Aramendia, Julene, Arana, Gorka, Bahia, Rickbir Singh, Banham, Steven G., Barnes, Robert, Barrett, Alexander M., Benedix, Wolf-Stefan, Bhardwaj, Anshuman, Boazman, Sarah Jane, Bontognali, Tomaso R. R., Bridges, John, Bultel, Benjamin, Ciarletti, Valérie, De Sanctis, Maria Cristina, Dickeson, Zach, Favaro, Elena A., Ferrari, Marco, Foucher, Frédéric, Goetz, Walter, Haldemann, Albert F. C., Harrington, Elise, Kapatza, Angeliki, Koschny, Detlef, Krzesinska, Agata M., Le Gall, Alice, Lewis, Stephen R., Lim, Tanya, Madariaga, Juan Manuel, Man, Benjamin James, Mandon, Lucia, Mangold, Nicolas, Martin-Torres, Javier, McNeil, Joseph D., Molina, Antonio, Moral, Andoni G., Motaghian, Sara, Nikiforov, Sergei, Oudart, Nicolas, Pacifici, Andrea, Parkes Bowen, Adam, Plettemeier, Dirk, Poulakis, Pantelis, Putri, Alfiah Rizky Diana, Ruesch, Ottaviano, Sam, Lydia, Schröder, Christian, Statz, Christoph, Thomas, Rebecca, Tirsch, Daniela, Toth, Zsuzsanna, Turner, Stuart, Voelker, Martin, Werner, Stephanie C., Westall, Frances, Whiteside, Barry J., Williams, Adam, Williams, Rebecca M. E., Wright, Jack, Zorzano, Maria-Paz, Fawdon, Peter, Orgel, Csilla, Adeli, Solmaz, Balme, Matt, Calef, Fred J., Davis, Joel M., Frigeri, Alessandro, Grindrod, Peter, Hauber, Ernst, Le Deit, Laetitia, Loizeau, Damien, Nass, Andrea, Quantin-Nataf, Cathy, Sefton-Nash, Elliot, Thomas, Nick, Torres, Ines, Vago, Jorge L., Volat, Matthieu, De Witte, Sander, Altieri, Francesca, Apuzzo, Andrea, Aramendia, Julene, Arana, Gorka, Bahia, Rickbir Singh, Banham, Steven G., Barnes, Robert, Barrett, Alexander M., Benedix, Wolf-Stefan, Bhardwaj, Anshuman, Boazman, Sarah Jane, Bontognali, Tomaso R. R., Bridges, John, Bultel, Benjamin, Ciarletti, Valérie, De Sanctis, Maria Cristina, Dickeson, Zach, Favaro, Elena A., Ferrari, Marco, Foucher, Frédéric, Goetz, Walter, Haldemann, Albert F. C., Harrington, Elise, Kapatza, Angeliki, Koschny, Detlef, Krzesinska, Agata M., Le Gall, Alice, Lewis, Stephen R., Lim, Tanya, Madariaga, Juan Manuel, Man, Benjamin James, Mandon, Lucia, Mangold, Nicolas, Martin-Torres, Javier, McNeil, Joseph D., Molina, Antonio, Moral, Andoni G., Motaghian, Sara, Nikiforov, Sergei, Oudart, Nicolas, Pacifici, Andrea, Parkes Bowen, Adam, Plettemeier, Dirk, Poulakis, Pantelis, Putri, Alfiah Rizky Diana, Ruesch, Ottaviano, Sam, Lydia, Schröder, Christian, Statz, Christoph, Thomas, Rebecca, Tirsch, Daniela, Toth, Zsuzsanna, Turner, Stuart, Voelker, Martin, Werner, Stephanie C., Westall, Frances, Whiteside, Barry J., Williams, Adam, Williams, Rebecca M. E., Wright, Jack, and Zorzano, Maria-Paz

Abstract

This 1:30,000 scale geological map describes Oxia Planum, Mars, the landing site for the ExoMars Rosalind Franklin rover mission. The map represents our current understanding of bedrock units and their relationships prior to Rosalind Franklin’s exploration of this location. The map details 15 bedrock units organised into 6 groups and 7 textural and surficial units. The bedrock units were identified using visible and near-infrared remote sensing datasets. The objectives of this map are (i) to identify where the most astrobiologically relevant rocks are likely to be found, (ii) to show where hypotheses about their geological context (within Oxia Planum and in the wider geological history of Mars) can be tested, (iii) to inform both the long-term (hundreds of metres to ∼1 km) and the short-term (tens of metres) activity planning for rover exploration, and (iv) to allow the samples analysed by the rover to be interpreted within their regional geological context.

12. The geography of Oxia Planum

Author

Fawdon, Peter, Grindrod, Peter, Orgel, Csilla, Sefton-Nash, Elliot, Adeli, Solmaz, Balme, Matt, Cremonese, Gabriele, Davis, Joel, Frigeri, Alessandro, Hauber, Ernst, Le Deit, Laetitia, Loizeau, Damien, Nass, Andrea, Parks-Bowen, Adam, Quantin-Nataf, Cathy, Thomas, Nick, Vago, Jorge L., Volat, Matthieu, Fawdon, Peter, Grindrod, Peter, Orgel, Csilla, Sefton-Nash, Elliot, Adeli, Solmaz, Balme, Matt, Cremonese, Gabriele, Davis, Joel, Frigeri, Alessandro, Hauber, Ernst, Le Deit, Laetitia, Loizeau, Damien, Nass, Andrea, Parks-Bowen, Adam, Quantin-Nataf, Cathy, Thomas, Nick, Vago, Jorge L., and Volat, Matthieu

Abstract

We present the geography of Oxia Planum, the landing site for the ExoMars 2022 mission. This map provides the planetary science community with a framework to understand this, until recently, unexplored area. The map comprises (1) a mosaic of the panchromatic Context Camera (CTX) Digital Elevation Models (DEM) and Ortho Rectified Images (ORI) controlled to the High Resolution Stereo Camera (HRSC) multiorbit Digital Elevation Models (DEM) and (2) a mosaic of Colour and Stereo Surface Imaging System (CaSSIS) synthetic colour data products, registered to the CTX ORI mosaic. We define a grid of exploration quadrangles (quads) and an informal group of geographic regions to describe Oxia Planum. These regions bridge the scale gap between features observed on large areas (∼100s km2) and the local geography (10s km2) relevant to the Rosalind Franklin rover’s operations in Oxia Planum.

13. Amazonian-aged fluvial system and associated ice-related features in Terra Cimmeria, Mars

Author

Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, Jaumann, Ralf, Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, and Jaumann, Ralf

Abstract

The Martian climate throughout the Amazonian is widely believed to have been cold and hyper-arid, very similar to the current conditions. However, ubiquitous evidence of aqueous and glacial activity has been recently reported, including channels that can be tens to hundreds of kilometres long, alluvial and fluvial deposits, ice-rich mantles, and glacial and periglacial landforms. Here we study a ∼340 km-long fluvial system located in the Terra Cimmeria region, in the southern mid-latitudes of Mars. The fluvial system is composed of an upstream catchment system with narrow glaciofluvial valleys and remnants of ice-rich deposits. We observe depositional features including fan-shaped deposits, and erosional features such as scour marks and streamlined islands. At the downstream section of this fluvial system is an outflow channel named Kārūn Valles, which displays a unique braided alluvial fan and terminates on the floor of the Ariadnes Colles basin. Our observations point to surface runoff of ice/snow melt as the water source for this fluvial activity. According to our crater size–frequency distribution analysis the entire fluvial system formed during early to middle Amazonian, between ∼1.8+0.2 −0.2 Ga to 510+40 −40 Ma. Hydraulic modelling indicates that the Kārūn Valles and consequently the alluvial fan formation took place in geologically short-term event(s). We conclude that liquid water was present in Terra Cimmeria during the early to middle Amazonian, and that Mars during that time may have undergone several episodic glacial-related events.

14. Amazonian-aged fluvial system and associated ice-related features in Terra Cimmeria, Mars

Author

Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, Jaumann, Ralf, Adeli, Solmaz, Hauber, Ernst, Kleinhans, Maarten, Le Deit, Laetitia, Platz, Thomas, Fawdon, Peter, and Jaumann, Ralf

Abstract

The Martian climate throughout the Amazonian is widely believed to have been cold and hyper-arid, very similar to the current conditions. However, ubiquitous evidence of aqueous and glacial activity has been recently reported, including channels that can be tens to hundreds of kilometres long, alluvial and fluvial deposits, ice-rich mantles, and glacial and periglacial landforms. Here we study a ∼340 km-long fluvial system located in the Terra Cimmeria region, in the southern mid-latitudes of Mars. The fluvial system is composed of an upstream catchment system with narrow glaciofluvial valleys and remnants of ice-rich deposits. We observe depositional features including fan-shaped deposits, and erosional features such as scour marks and streamlined islands. At the downstream section of this fluvial system is an outflow channel named Kārūn Valles, which displays a unique braided alluvial fan and terminates on the floor of the Ariadnes Colles basin. Our observations point to surface runoff of ice/snow melt as the water source for this fluvial activity. According to our crater size–frequency distribution analysis the entire fluvial system formed during early to middle Amazonian, between ∼1.8+0.2 −0.2 Ga to 510+40 −40 Ma. Hydraulic modelling indicates that the Kārūn Valles and consequently the alluvial fan formation took place in geologically short-term event(s). We conclude that liquid water was present in Terra Cimmeria during the early to middle Amazonian, and that Mars during that time may have undergone several episodic glacial-related events.

15. The geography of Oxia Planum

Author

Fawdon, Peter, Grindrod, Peter, Orgel, Csilla, Sefton-Nash, Elliot, Adeli, Solmaz, Balme, Matt, Cremonese, Gabriele, Davis, Joel, Frigeri, Alessandro, Hauber, Ernst, Le Deit, Laetitia, Loizeau, Damien, Nass, Andrea, Parks-Bowen, Adam, Quantin-Nataf, Cathy, Thomas, Nick, Vago, Jorge L., Volat, Matthieu, Fawdon, Peter, Grindrod, Peter, Orgel, Csilla, Sefton-Nash, Elliot, Adeli, Solmaz, Balme, Matt, Cremonese, Gabriele, Davis, Joel, Frigeri, Alessandro, Hauber, Ernst, Le Deit, Laetitia, Loizeau, Damien, Nass, Andrea, Parks-Bowen, Adam, Quantin-Nataf, Cathy, Thomas, Nick, Vago, Jorge L., and Volat, Matthieu

Abstract

We present the geography of Oxia Planum, the landing site for the ExoMars 2022 mission. This map provides the planetary science community with a framework to understand this, until recently, unexplored area. The map comprises (1) a mosaic of the panchromatic Context Camera (CTX) Digital Elevation Models (DEM) and Ortho Rectified Images (ORI) controlled to the High Resolution Stereo Camera (HRSC) multiorbit Digital Elevation Models (DEM) and (2) a mosaic of Colour and Stereo Surface Imaging System (CaSSIS) synthetic colour data products, registered to the CTX ORI mosaic. We define a grid of exploration quadrangles (quads) and an informal group of geographic regions to describe Oxia Planum. These regions bridge the scale gap between features observed on large areas (∼100s km2) and the local geography (10s km2) relevant to the Rosalind Franklin rover’s operations in Oxia Planum.

Catalog

Books, media, physical & digital resources
See catalog results