Zobrazeno 1 - 10
of 37
pro vyhledávání: '"Butcher, F.E.G."'
Publikováno v:
In Icarus 1 September 2024 419
Publikováno v:
In Icarus October 2022 385
Autor:
Balme, M.R., Curtis-Rouse, M.C., Banham, S., Barnes, D., Barnes, R., Bauer, A., Bedford, C.C., Bridges, J.C., Butcher, F.E.G., Caballo-Perucha, P., Caldwell, A., Coates, A.J., Cousins, C., Davis, J.M., Dequaire, J., Edwards, P., Fawdon, P., Furuya, K., Gadd, M., Get, P., Griffiths, A., Grindrod, P.M., Gunn, M., Gupta, S., Hansen, R., Harris, J.K., Hicks, L.J., Holt, J., Huber, B., Huntly, C., Hutchinson, I., Jackson, L., Kay, S., Kyberd, S., Lerman, H.N., McHugh, M., McMahon, W.J., Muller, J.-P., Ortner, T., Osinski, G., Paar, G., Preston, L.J., Schwenzer, S.P., Stabbins, R., Tao, Y., Traxler, C., Turner, S., Tyler, L., Venn, S., Walker, H., Wilcox, T., Wright, J., Yeomans, B.
Publikováno v:
In Planetary and Space Science January 2019 165:31-56
Publikováno v:
Earth Surface Processes & Landforms; Nov2023, Vol. 48 Issue 14, p2754-2771, 18p
Autor:
Woodley, S.Z., Butcher, F.E.G., Fawdon, P., Clark, C.D., Ng, F.S.L., Davis, J.M., Gallagher, C.
Precipitation in Mars' mid-latitudes formed Viscous Flow Features (VFFs), landforms analogous to terrestrial debris-covered glaciers, in the last 1 Gyr. Until recently, the prevailing view was that the Amazonian environment was not conducive to basal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::4f7cdacc2b4552a3a49dcc264495afcb
https://eprints.whiterose.ac.uk/188750/1/1-s2.0-S0019103522002500-main.pdf
https://eprints.whiterose.ac.uk/188750/1/1-s2.0-S0019103522002500-main.pdf
Autor:
Butcher, F.E.G., Balme, M.R., Conway, S.J., Gallagher, C., Arnold, N.S., Storrar, R.D., Lewis, S.R., Hagermann, A.
We present a systematic, metre-scale characterisation of the 3D morphometry of an esker on Mars, and the first attempt to reconstruct the multi-stage dynamics of esker formation on Mars. Eskers are sinuous ridges comprising sediment deposited by melt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::313793bf894d4f8798510bf8c747907d
https://eprints.whiterose.ac.uk/160823/58/1-s2.0-S0012821X20302697-main.pdf
https://eprints.whiterose.ac.uk/160823/58/1-s2.0-S0012821X20302697-main.pdf
The mid- to high latitudes of Mars host assemblages of landforms consistent with a receding glacial landscape on Earth. These landforms are postulated to have formed >5 Ma under a different climate regime when Mars' orbital obliquity was on average 1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::8400705ecd68cc85c9dd6d6e369b8521
Autor:
Butcher, F.E.G., Balme, M.R., Gallagher, C., Arnold, N.S., Conway, S.J., Hagermann, A., Lewis, S.R.
Publikováno v:
Journal of Geophysical Research. Planets
Journal of Geophysical Research. Planets, Wiley-Blackwell, 2017, 122 (12), pp.2445-2468. ⟨10.1002/2017JE005434⟩
Journal of Geophysical Research. Planets, Wiley-Blackwell, 2017, 122 (12), pp.2445-2468. ⟨10.1002/2017JE005434⟩
International audience; Evidence for past basal melting of young (late Amazonian-aged), debris-covered glaciers in Mars' mid-latitudes is extremely rare. Thus, it is widely thought that these viscous flow features (VFFs) have been perennially frozen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::f4bbc311018313a755bc74723960ee88
https://eprints.whiterose.ac.uk/149878/1/Butcher_et_al-2017-Journal_of_Geophysical_Research__Planets.pdf
https://eprints.whiterose.ac.uk/149878/1/Butcher_et_al-2017-Journal_of_Geophysical_Research__Planets.pdf
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Akademický článek
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