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Philippe Lognonné

Researcher at Institut de Physique du Globe de Paris

Publications -  253
Citations -  10503

Philippe Lognonné is an academic researcher from Institut de Physique du Globe de Paris. The author has contributed to research in topics: Mars Exploration Program & Seismometer. The author has an hindex of 48, co-authored 216 publications receiving 7229 citations. Previous affiliations of Philippe Lognonné include Paris-Sorbonne University & University of Paris.

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Seismic detection of the lunar core

TL;DR: Reinterpreted Apollo-era seismic data from the Moon reveal a solid inner core and a fluid outer core, overlain by a partially molten boundary layer, consistent with a volatile-depleted interior.
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Initial results from the InSight mission on Mars

W. Bruce Banerdt, +76 more
- 24 Feb 2020 - 
TL;DR: For example, the first ten months of the InSight lander on Mars revealed a planet that is seismically active and provided information about the interior, surface and atmospheric workings of Mars as mentioned in this paper.
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Ionospheric detection of gravity waves induced by tsunamis

TL;DR: In this paper, the authors used the GEONET network in Japan to image small-scale perturbations of the Total Electron Content above Japan and up to 400 km off shore.
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SEIS: Insight’s Seismic Experiment for Internal Structure of Mars

Philippe Lognonné, +186 more
TL;DR: The science goals of the experiment and the rationale used to define its requirements are described, and the hardware, from the sensors to the deployment system and associated performance, including transfer functions of the seismic sensors and temperature sensors are described.
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A new seismic model of the Moon: implications for structure, thermal evolution and formation of the Moon

TL;DR: In this paper, the authors determined a new seismic model of the Moon after a complete independent reprocessing of the Apollo lunar seismic data with determination of arrival times of about 60 natural and artificial lunar quakes, as well as travel times of converted phases at the crust-mantle interface below the Apollo 12 landing site.