Homothéties de figures à 5 sommets par rapport à l'origine -- 1er quadrant (A)

Our analysis shows that the poroelastic response to ocean tidal loading is controlled by the permeability structure of extrusive layer 2A, which varies considerably across sites

(a) Orthorectified mosaic obtained by projecting DISR images using the positions and orientations from the SPICE kernels only, (b) orthorectified mosaic obtained from the po- sition

High temperature impact melt breccias from the Rochechouart (France) meteorite crater record a magnetization component with antipodal, normal and reverse polarities.. The

The introduction of MCF into compressive detector, which is termed as mCPM here, could be very promising in our particular case and can also facilitate parameter adjustment with

Conventional synthetic aperture radar imaging techniques mainly achieving focused radar imaging is based on the physical-mathematical model that the radar received signal is sum of

From 0 day to 14 days, the dissolution rate of precursors increases (Figure 11), simultaneously, the mean crystal size increases (Figure 7b) and small particles continuously

Sci. Detection of small hydrological variations in gravity by repeated observations with relative gravimeters, J. Present-day interseismic surface deformation along the

To update the use of bio-based glycolaldehyde, a hydrolysis product of cellulose or glucose, as a platform molecule towards value-added products, we first