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Meter-scale thermal contraction crack polygons on the nucleus of comet 67P/Churyumov-Gerasimenko
A.-T. Auger, O. Groussin, L. Jorda, M.R. El-Maarry, S. Bouley, A. Séjourné, R. Gaskell, C. Capanna, B. Davidsson, S. Marchi, S. Höfner, P.L. Lamy, H. Sierks, C. Barbieri, R. Rodrigo, D. Koschny, H. Rickman, H.U. Keller, J. Agarwal, M.F. A’Hearn, M.A. Barucci, J.-L. Bertaux, I. Bertini, G. Cremonese, V. Da Deppo, et al. Icarus 301 173 (2018) https://doi.org/10.1016/j.icarus.2017.09.037
Evolution of CO2, CH4, and OCS abundances relative to H2O in the coma of comet 67P around perihelion fromRosetta/VIRTIS-H observations
Dominique Bockelée-Morvan, J. Crovisier, S. Erard, et al. Monthly Notices of the Royal Astronomical Society 462(Suppl 1) S170 (2016) https://doi.org/10.1093/mnras/stw2428
Sulphur-bearing species in the coma of comet 67P/Churyumov–Gerasimenko
U. Calmonte, K. Altwegg, H. Balsiger, et al. Monthly Notices of the Royal Astronomical Society 462(Suppl 1) S253 (2016) https://doi.org/10.1093/mnras/stw2601
Unexpected and significant findings in comet 67P/Churyumov–Gerasimenko: an interdisciplinary view
Marco Fulle, N. Altobelli, B. Buratti, et al. Monthly Notices of the Royal Astronomical Society 462(Suppl 1) S2 (2016) https://doi.org/10.1093/mnras/stw1663
Permittivity measurements of porous matter in support of investigations of the surface and interior of 67P/Churyumov-Gerasimenko
IDIS Small Bodies and Dust Node: Technical innovation and science
M. Giardino, V.F. Braga, M.C. De Sanctis, L. Giacomini, S. Giuppi, D. Turrini and M.T. Capria Advances in Space Research 55(2) 747 (2015) https://doi.org/10.1016/j.asr.2014.10.029
First observations of H2O and CO2vapor in comet 67P/Churyumov-Gerasimenko made by VIRTIS onboard Rosetta
On the conditions for fluidisation in cometary mantles
Mark S. Bentley, Norbert I. Kömle, Günter Kargl, Erika Kaufmann and Erika Hütter Advances in Space Research 48(5) 862 (2011) https://doi.org/10.1016/j.asr.2011.04.039
SEASONAL EFFECTS ON COMET NUCLEI EVOLUTION: ACTIVITY, INTERNAL STRUCTURE, AND DUST MANTLE FORMATION