Seismic tomography enables to model the internal structure of the Earth. The analysis of huge amounts of data leads to improvements in the precisio n of models. 1 juil. Sismicité et géométrie de l’interplaque 3 Sismique marine grand-angle et tomographie. Acquisition: sismique. 3 janv. d’autres laboratoires européens, les méthodes de sismique active et tomographie sismique en ondes SH et par inversion des ondes de.

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Calcul de rais en tomographie sismique. Exploitation sur la grille

Zones de subduction horizontale versus normale: By clicking accept or continuing to use the site, you agree to the terms outlined in our Privacy PolicyTerms of Serviceand Dataset License. In upstream of the alluvial plain, near the river, these methods were used to map the sandy to sandy-thin deposits m and the unfractured bedrock.

From This Paper Figures, tables, and topics from this paper. We tmoographie significant seismic differences between the flat and normal subduction zones.

Tuesday, December 11, – 1: Ray tracing graphics Search for additional papers on this topic. As expected, the flat slab region is impacted by colder temperatures, and therefore by faster seismic velocities and more intense seismic activity, compared to the normal slab region.


Marianne Marot 1 AuthorId: GeorgeJohn G.

O pen R epository and Bi bliography. Tomography Central processing unit.

In this basin, the main surface water resource for agricultural needs is constituted by a small perennial river, but in recent years this resource is insufficient to satisfy the uses in agriculture. The analysis of huge amounts of data leads to improvements in the precisio n of models but requires massive computations. Xismique aquifer could be easily accessible with rudimentary structures such as sumps and could constitute a supplementary water source, simique irrigation activities in this second region of Burkina Faso.

FosterNicholas T. Downstream they highlight fractured and deconsolidated bedrock drawing a V-shaped geometry of deposits.

The aim of our study is to assess, using a thermo-petrological-seismological approach, the differences of the overriding lithosphere between these two regions, in order to better understand the deep structure of the continental lithosphere above the flat slab, and the links between the deformations at the surface and at depth.

We confirm previous studies that have shown that the thick lower crust of the present day Andean arc is non-eclogitized and maybe representing the felsic Chilenia terrane, whereas to the east, the Cuyania terrane in the backarc is more mafic and contains an eclogitized lower crust.

We show evidence that the flat slab dehydrates within the mantle wedge, but also along sismiqhe subducting ridge prior to re-subducting. The alluvial plain would be relatively thicker downstream of the study area approximately 30 to 50m. Citations Publications citing this paper. Have you forgotten your login?


Calcul de rais en tomographie sismique. Exploitation sur la grille – Semantic Scholar

The continental crust above the flat slab has very heterogeneous seismic properties which correlate with important deformation structures and geological terranes at the surface. Bandwidthcentric allocation of independent tasks on heterogeneous platforms. Calcul de rais en tomographie sismique.

Thursday, December 12, – 1: Skip to search form Skip to main content. References Publications referenced by this paper. HagedornJudith Ellen Devaney Marianne Marot 1 Details.

tomographie sismique et électrique

This geometry is due to the faults and the magmatic intrusions. Linear algebra Telecommuting Grid computing. All documents in ORBi are protected by a user license.

Topics Discussed in This Paper. In International Parallel and Distributed…. Thursday, March 13, – 5: Hagedornand Judith E.