Search Results - "Mainsant, G."

Monitoring Saturation Changes with Ambient Seismic Noise and Gravimetry in a Karst Environment by Fores, B., Champollion, C., Mainsant, G., Albaric, J., Fort, A.

“…Core Ideas Saturation changes can be monitored with ambient seismic noise. We present a new and nondestructive tool to investigate deep and heterogeneous…”
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Shear-wave velocity as an indicator for rheological changes in clay materials: Lessons from laboratory experiments by Mainsant, G., Jongmans, D., Chambon, G., Larose, E., Baillet, L.

“…Clay‐rich geological formations are responsible for many landslides, the dynamics of which are still poorly understood and intensely debated. Analysis of…”
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Autocorrelation of the Ground Vibrations Recorded by the SEIS‐InSight Seismometer on Mars by Compaire, N., Margerin, L., Garcia, R. F., Pinot, B., Calvet, M., Orhand‐Mainsant, G., Kim, D., Lekic, V., Tauzin, B., Schimmel, M., Stutzmann, E., Knapmeyer‐Endrun, B., Lognonné, P., Pike, W. T., Schmerr, N., Gizon, L., Banerdt, W. B.

“…Since early February 2019, the SEIS (Seismic Experiment for Interior Structure) seismometer deployed at the surface of Mars in the framework of the InSight…”
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A Comodulation Analysis of Atmospheric Energy Injection Into the Ground Motion at InSight, Mars by Charalambous, C., Stott, A. E., Pike, W. T., McClean, J. B., Warren, T., Spiga, A., Banfield, D., Garcia, R. F., Clinton, J., Stähler, S., Navarro, S., Lognonné, P., Scholz, J.‐R., Kawamura, T., van Driel, M., Böse, M., Ceylan, S., Khan, A., Horleston, A., Orhand‐Mainsant, G., Sotomayor, L. M., Murdoch, N., Giardini, D., Banerdt, W. B.

“…Seismic observations involve signals that can be easily masked by noise injection. For the NASA Mars lander InSight, the atmosphere is a significant noise…”
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Hydroacoustic monitoring of a salt cavity: an analysis of precursory events of the collapse by Lebert, F., Bernardie, S., Mainsant, G.

“…One of the main features of "post mining" research relates to available methods for monitoring mine-degradation processes that could directly threaten surface…”
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The seismicity of Mars by Giardini, D., Lognonné, P., Banerdt, W. B., Pike, W. T., Christensen, U., Ceylan, S., Clinton, J. F., van Driel, M., Stähler, S. C., Böse, M., Garcia, R. F., Khan, A., Panning, M., Perrin, C., Banfield, D., Beucler, E., Charalambous, C., Euchner, F., Horleston, A., Jacob, A., Kawamura, T., Kedar, S., Mainsant, G., Scholz, J.-R., Smrekar, S. E., Spiga, A., Agard, C., Antonangeli, D., Barkaoui, S., Barrett, E., Combes, P., Conejero, V., Daubar, I., Drilleau, M., Ferrier, C., Gabsi, T., Gudkova, T., Hurst, K., Karakostas, F., King, S., Knapmeyer, M., Knapmeyer-Endrun, B., Llorca-Cejudo, R., Lucas, A., Luno, L., Margerin, L., McClean, J. B., Mimoun, D., Murdoch, N., Nimmo, F., Nonon, M., Pardo, C., Rivoldini, A., Manfredi, J. A. Rodriguez, Samuel, H., Schimmel, M., Stott, A. E., Stutzmann, E., Teanby, N., Warren, T., Weber, R. C., Wieczorek, M., Yana, C.

“…The InSight (Interior Exploration using Seismic Investigations, Geodesy and Heat Transport) mission landed in Elysium Planitia on Mars on 26 November 2018 and…”
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Seasonal seismic activity on Mars by Knapmeyer, M., Stähler, S.C., Daubar, I., Forget, F., Spiga, A., Pierron, T., van Driel, M., Banfield, D., Hauber, E., Grott, M., Müller, N., Perrin, C., Jacob, A., Lucas, A., Knapmeyer-Endrun, B., Newman, C., Panning, M.P., Weber, R.C., Calef, F.J., Böse, M., Ceylan, S., Charalambous, C., Clinton, J., Dahmen, N., Giardini, D., Horleston, A., Kawamura, T., Khan, A., Mainsant, G., Plasman, M., Lemmon, M., Lorenz, R., Pike, W.T., Scholz, J.-R., Lognonné, P., Banerdt, B.

“…•InSight SEIS finds seasonal variations of “High Frequency” type Marsquake occurrence.•Likely driving forces are solar illumination, the CO2 ice cycle, or…”
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Shear-wave-velocity drop prior to clayey mass movement in laboratory flume experiments by Mainsant, Guénolé, Chambon, Guillaume, Jongmans, Denis, Larose, Eric, Baillet, Laurent

“…Clay slopes are susceptible to suddenly liquefy into rapidly accelerating landslides, thereby threatening people and facilities in mountainous areas. Because…”
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