CanMars mission Science Team operational results: Implications for operations and the sample selection process for Mars Sample Return (MSR)

Autor: S. L. Simpson, Gordon R. Osinski, Anna Grau Galofre, E. Godin, Livio L. Tornabene, J. T. Poitras, C. M. Caudill, Anna Mittelholz, Melissa Battler, R. Francis, Matthew Svensson, V. Hipkin, Z. R. Morse, T. Haltigin, Eric A. Pilles, Alexandra Pontefract, Tianqi Xie

Publikováno v: Planetary and Space Science. 172:43-56

The CanMars Mars sample return (MSR) analogue mission was conducted as a field and operational test for the Mars 2020 sample cache rover mission and was the most realistic known MSR rover analogue mission to-date. A rover — similar in scale to that

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::43c1cb923e55cc9c3e2e62b22e6d093f
https://doi.org/10.1016/j.pss.2019.04.004

The CanMars Mars Sample Return analogue mission

Autor: Derek King, T. Haltigin, A. Bina, C. L. Marion, Jackie Goordial, Racel Sopoco, E. A. Lymer, Tom Dzamba, Anna Grau Galofre, E. M. Harrington, Martin Picard, R. Francis, K. Balachandran, C. M. Caudill, Liam Robert John Innis, P. A. Christoffersen, S. Duff, Elizabeth A. Silber, Alexandra Pontefract, Joshua Laughton, Rebecca Wilks, M. C. Kerrigan, Yaozhu Li, Edward A. Cloutis, Dylan Hickson, Daniel Bednar, Kristen Cote, C. H. Ryan, Tanya N. Harrison, Omar Draz, M. Bourassa, Tianqi Xie, Paul Fulford, Melissa Battler, Ian Pritchard, J. W. O’Callaghan, E. Godin, Eric A. Pilles, Matthew Svensson, Matthew Maloney, Sarah Mcfadden, Matthew Cross, P. Patel, David Beaty, J. D. Newman, John Maris, Scott M. McLennan, Kenneth H. Williford, Pierre Allard, Fenge Cao, Haley M. Sapers, Alexis David P. Pascual, Bryce Dudley, Diego Uribe, V. Hipkin, Z. R. Morse, Anna Mittelholz, Taylor Haid, W. Zylberman, Bianca D'Aoust, Catherine Maggiori, J. T. Poitras, Byung-Hun Choe, Gordon R. Osinski, Livio L. Tornabene, J. Hawkswell, P. J. A. Hill, Jonathan Kissi, G. D. Tolometti, S. L. Simpson, Joseph Nsasi Bakambu

Publikováno v: Planetary and Space Science. 166:110-130

The return of samples from known locations on Mars is among the highest priority goals of the international planetary science community. A possible scenario for Mars Sample Return (MSR) is a series of 3 missions: sample cache, fetch, and retrieval. T

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::037955d995fd47d54bfbebf5126f9c11
https://doi.org/10.1016/j.pss.2018.07.011

Exploring new models for improving planetary rover operations efficiency through the 2016 CanMars Mars Sample Return (MSR) analogue deployment

Autor: Scott M. McLennan, J. D. Newman, M. C. Kerrigan, Kenneth H. Williford, R. Francis, Melissa Battler, M. Bourassa, T. Haltigin, C. M. Caudill, Elizabeth A. Silber, Eric A. Pilles, Matthew Cross, V. Hipkin, Gordon R. Osinski

Publikováno v: Planetary and Space Science. 165:250-259

Approaches to rover mission operations were investigated in the framework of the CanMars Mars Sample Return (MSR) analogue mission deployments. Improving the efficiency of operations is a necessity for future planetary missions, including Mars 2020,

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::e0fd28355e498aa576dcb99f1a032b32
https://doi.org/10.1016/j.pss.2018.10.001

Formation of large-scale impact melt dikes: A case study of the Foy Offset Dike at the Sudbury impact structure, Canada

Autor: Eric A. Pilles, Joshua Bailey, Gordon R. Osinski, David E. Smith, Richard A. F. Grieve

Publikováno v: Earth and Planetary Science Letters. 495:224-233

Hypervelocity impacts frequently result in the formation of dikes in the crater floor and central uplift. Impact melt-bearing dikes in large terrestrial impact basins – such as the Offset Dikes at the Sudbury impact structure – occur at a large s

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::214b7e99103c21507c060db525847789
https://doi.org/10.1016/j.epsl.2018.05.023

Igneous rocks formed by hypervelocity impact

Autor: Richard A. F. Grieve, Livio L. Tornabene, Gordon R. Osinski, Eric A. Pilles, Jacob E. Bleacher, Catherine D. Neish

Publikováno v: Journal of Volcanology and Geothermal Research. 353:25-54

Igneous rocks are the primary building blocks of planetary crusts. Most igneous rocks originate via decompression melting and/or wet melting of protolith lithologies within planetary interiors and their classification and compositional, petrographic,

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::72b20cc1d58054b39c2b39b0554dfc0a
https://doi.org/10.1016/j.jvolgeores.2018.01.015