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Caroline Freissinet

Researcher at Université Paris-Saclay

Publications -  87
Citations -  4935

Caroline Freissinet is an academic researcher from Université Paris-Saclay. The author has contributed to research in topics: Sample Analysis at Mars & Mars Exploration Program. The author has an hindex of 23, co-authored 73 publications receiving 3742 citations. Previous affiliations of Caroline Freissinet include University of Maryland, Baltimore County & Centre national de la recherche scientifique.

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Organic molecules in the Sheepbed Mudstone, Gale Crater, Mars

TL;DR: Chlorinated hydrocarbons identified in the Sheepbed mudstone by SAM are the reaction products of Martian chlorine and organic carbon derived from Martian sources or exogenous sources such as meteorites, comets, or interplanetary dust particles.
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Evidence for perchlorates and the origin of chlorinated hydrocarbons detected by SAM at the Rocknest aeolian deposit in Gale Crater

TL;DR: A single scoop of the Rocknest aeolian deposit was sieved and four separate sample portions, each with a mass of ~50mg, were delivered to individual cups inside the Sample Analysis at Mars (SAM) instrument by the Mars Science Laboratory rover's ample acquisition system.
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Curiosity at Gale Crater, Mars: Characterization and Analysis of the Rocknest Sand Shadow

David F. Blake, +44 more
- 27 Sep 2013 - 
TL;DR: The Rocknest aeolian deposit is similar to aeOLian features analyzed by the Mars Exploration Rovers Spirit and Opportunity and implies locally sourced, globally similar basaltic materials or globally and regionally sourced basALTic components deposited locally at all three locations.
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Background levels of methane in Mars' atmosphere show strong seasonal variations

TL;DR: In situ measurements at Gale crater made over a 5-year period by the Tunable Laser Spectrometer on the Curiosity rover show large seasonal variation in the background and occurrences of higher temporary spikes that are consistent with small localized sources of methane released from martian surface or subsurface reservoirs.