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2012 (v1)Journal articleUploaded on: December 2, 2022
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2010 (v1)Journal article
International audience
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2010 (v1)Journal article
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Uploaded on: December 4, 2022 -
2007 (v1)Journal article
Icarus, 188, pp. 468-480, http://dx.doi.org./10.1016/j.icarus.2006.11.018
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2010 (v1)Journal article
Nature, 465, pp. 752-754 (2010)
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2010 (v1)Journal article
Nature, 465, pp. 752-754 (2010)
Uploaded on: February 22, 2023 -
2009 (v1)Journal article
Icarus, 199, pp. 413-428, http://dx.doi.org./10.1016/j.icarus.2008.10.019
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2010 (v1)Journal article
International audience
Uploaded on: December 3, 2022 -
2010 (v1)Journal article
International audience
Uploaded on: December 3, 2022 -
January 2022 (v1)Journal article
The formation of planetesimals is expected to occur via particle-gas instabilities that concentrate dust into self-gravitating clumps. Triggering these instabilities requires the prior pile-up of dust in the protoplanetary disk. This has been successfully modelled exclusively at the disk's snowline, whereas rocky planetesimals in the inner disk...
Uploaded on: December 3, 2022 -
September 17, 2017 (v1)Conference paper
The Hera Saturn entry probe mission is proposed as an ESA M-class mission to be piggybacked on a NASA spacecraft sent to or past the Saturn system. Hera consists of an atmospheric probe built by ESA and released into the atmosphere of Saturn by its NASA companion Saturn Carrier-Relay spacecraft. Hera will perform in situ measurements of the...
Uploaded on: February 28, 2023 -
September 17, 2017 (v1)Conference paper
Uranus and Neptune, referred to as ice giants, are fundamentally different from the better-known gas giants (Jupiter and Saturn). Exploration of an ice giant system is a high-priority science objective, as these systems (including the magnetosphere, satellites, rings, atmosphere, and interior) challenge our understanding of planetary formation...
Uploaded on: February 28, 2023