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13篇 您的检索式：作者名="Baratoux"

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		题名	作者	年代	出处	被引量
	1	Surface Motion of M ountain Glaciers Derived from Satellite Optical Imagery显示文摘	Berthier E Vadon H Baratoux D	2005	Remote Sensing of Environment2005，95，1：	1
	2	Surface motion of mountain glaciers derived from satellite optical imagery显示文摘	Berthier E Vadon H Baratoux D	2005	Remote Sensing of Environment2005，95，1：	1
	3	Recent rapid thinning of the'Mer de Glace'glacier derived from satellite optical images显示文摘	BERTHIER E ARNAUD Y BARATOUX D	2004	Geophysical Research Letters2004，31，：	1
	4	Surface motion of mountain glaciers derived from satellite optical imagery显示文摘	Berthier E Vadon H Baratoux D	2005	Re- mote Sensing of Environment2005，95，：	1
	5	Surface motion of mountain glaciers derived from satellite optical imagery显示文摘	Berthier E Vadon H Baratoux D	2005	Remote Sensing of Environment2005，95，1：	1
	6	Reconstructing the total shortening history of the NW Himalaya显示文摘	Guillot S Garzanti E Baratoux D	2003	Geochemistry Geophys- ics Geosystems2003，4，7：	1
	7	The quantitative link between fold geometry, mineral fabric and mechanical anisotropy; as exemplified by the deformation of amphibolites across a regional metamorphic gradient 显示文摘	Baratoux L Lexa O Cosgrove J W	2005	Journal of Structural Geology2005，27，4：	1
	8	Surface roughness and geological mapping at subhectometer scale from the High Resolution Stereo Camera onboard Mars Express显示文摘	Aurélien Cord David Baratoux Nicolas Mangold Patrick Martin Patrick Pinet Ronald Greeley Francois Costard Philippe Masson Bernard Foing Gerhard Neukum	2007	Icarus2007，，1：	1
	9	Surface motion of mountain glaciers derived from satellite optical imagery显示文摘	Berthier E Vadon H Baratoux D	2005	Remote Sensing of Environment2005，95，1：	1
	10	Seventeen years of the “La Clapière” landslide evolution analysed from ortho-rectified aerial photographs显示文摘	B. Casson C. Delacourt D. Baratoux P. Allemand	2002	Engineering Geology2002，，1：	1
	11	Surface Roughness and Geo-logical Mapping at Subhectometer Scale from the High ResolutionStereo Camera Onboard Mars Express显示文摘	Cord A Baratoux D Mangold N	2007	Icarus2007，191，1：	1
	12	Seventeen Years of the “La Clapiere” Landslide Evolution Analysed from Ortho- rectified Aerial Photographs 显示文摘	Casson B Delacourt C Baratoux D	2003	Engineering Geology2003，68，：	1
	13	Development and Evolution of the Size of Polygonal Fracture Systems during Fluid-Solid Separation in Clay-Rich Deposits显示文摘In continental and oceanic conditions, clay-rich deposits are characterised by the development of polygonal fracture systems(PFS). PFS can increase the vertical permeability of clay-rich deposits(mean permeability ≤10^(-16) m^2) and are pathways for fluids. On continents, the width of PFS ranges from centimeters to hundreds of meters, while in oceanic contexts they are up to a few kilometers large. These structures are linked to water-solid separation during deposition, consolidation and complete fluid squeeze of the clay horizon. During the last few decades, modeling of melt migration in partially molten plastic rocks led to rigorous quantifications of two-phase flows with a particular emphasis on 2D and 3D induced flow structures. The numerical modeling shows that the melt migrates on distances almost equal to a few times the compaction length L that depends on permeability and viscosity. Consequently, polygonal structures in partially molten plastic rocks are resulted from the melt-rock separation and their sizes are proportional to L. Applying these results to fluid-solid separation in clay-rich horizons, we show that(1) centimetric to kilometric PFS are resulted from the dramatic increase of L during compaction and(2), this process involves agglomerates with 100 μm to 1 mm size.	Teodolina Lopez Raphael Antoine JoséDarrozes Michel Rabinowicz David Baratoux	2018	Journal of Earth Science2018，29，6：	1

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