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Claire Capanna

Researcher at Aix-Marseille University

Publications -  23
Citations -  1510

Claire Capanna is an academic researcher from Aix-Marseille University. The author has contributed to research in topics: Comet & Ultimate tensile strength. The author has an hindex of 11, co-authored 23 publications receiving 1338 citations.

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On the nucleus structure and activity of comet 67P/Churyumov-Gerasimenko

Holger Sierks, +70 more
- 23 Jan 2015 - 
TL;DR: Images from the OSIRIS scientific imaging system onboard Rosetta show that the nucleus of 67P/Churyumov-Gerasimenko consists of two lobes connected by a short neck, which raises the question of whether the two Lobes represent a contact binary formed 4.5 billion years ago, or a single body where a gap has evolved via mass loss.
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The global shape, density and rotation of Comet 67P/Churyumov-Gerasimenko from preperihelion Rosetta/OSIRIS observations

TL;DR: In this article, a high-resolution shape model of the nucleus of the comet 67P/Churyumov-Gerasimenko was used to estimate the porosity of the surface of the cometary nucleus.
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Large heterogeneities in comet 67P as revealed by active pits from sinkhole collapse

Jean-Baptiste Vincent, +67 more
- 02 Jul 2015 - 
TL;DR: It is reported that pits on comet 67P/Churyumov–Gerasimenko are active, and probably created by a sinkhole process, possibly accompanied by outbursts, and argued that after formation, pits expand slowly in diameter, owing to sublimation-driven retreat of the walls.
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Two independent and primitive envelopes of the bilobate nucleus of comet 67P

Matteo Massironi, +59 more
- 15 Oct 2015 - 
TL;DR: The notable structural similarities between the two lobes of comet 67P/Churyumov–Gerasimenko indicate that the early-forming cometesimals experienced similar primordial stratified accretion, even though they formed independently.
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Gravitational slopes, geomorphology, and material strengths of the nucleus of comet 67P/Churyumov-Gerasimenko from OSIRIS observations

TL;DR: In this paper, the tensile, shear, and compressive strengths of the cometary material were estimated using different surface morphologies (overhangs, collapsed structures, boulders, cliffs, and Philae's footprint) and mechani- cal considerations.