Abhatoo : Activités sismiques

Auteur : Chabli Ahmed, Bargach Kaoutar, Chalouan Ahmed

Mise en évidence d’une tectonique distensive associée à la convergence Eurasie-Afrique dans le Nord de la Meseta occidental marocaine durant le Plio-Quaternaire

La Meseta côtière marocaine fait partie de la marge passive du Maroc. La présente étude est menée dans une partie de cette marge passive, entre Rab...

Auteur : Boukhal A., Lferde M., Cherkaoui T.-E. ...[et al.] Samedi 13 Mars 1999

Activité sismique et signal radon: Cas de quelques séismes de magnitude supérieure à 5

Ce travail présente le comportement du radon émanant du sol dans quatre régions du Maroc (Tétouan, Khouribga, Ifrane et Berchid) vis à vis de deux...

Auteur : Meibom Anders, Anderson Don L.

The Statistical Upper Mantle Assemblage

A fundamental challenge in modern mantle geochemistry is to link geochemical data with geological and geophysical observations. Earlier efforts ha...

Auteur : Cooper C. M., Conrad Clinton P. Dimanche 05 Juillet 2009

Does the mantle control the maximum thickness of cratons ?

Geochemical observations suggest that cratonic xenoliths originate from depths no greater than 250 km, which implies a maximum craton thickness. W...

Auteur : Bindeman I.N., Schmitt A.K., Evans D.A.D.

Limits of hydrosphere-lithosphere interaction: Origin of the lowestknown δ18O silicate rock on Earth in the Paleoproterozoic Karelian rift

Geologic records of Earth’s hydrosphere and meteoric precipitation older than 2 Ga are rare, although they provide insight into the past climate,...

Auteur : Wolf Detlef

A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt

The study proposes an inversion method applicable to observations of deglacial land uplift and tilt near the margin of a major Pleistocene ice-she...

Auteur : Aumento F. Jeudi 25 Novembre 2010

Distribution and Evolution of Uranium in the Oceanic Lithosphere

Induced fission track techniques permit us to determine quantitatively the micro-scopic distribution of uranium in rocks, in their constituent min...

Auteur : Ebbing Jörg, Olesen Odleiv, Lauritsen Torleif, ...[et al.] Mardi 01 Juin 2010

Isostatic state and density structure from surface to depth of the lithosphere below the Norwegian continental margin

Summary Top basement and Moho geometry reflect the tectonic evolution of the Northeast Atlantic margin – Gravity and magnetic are especially h...

Auteur : Hetland E.A., Moore S.B. Mardi 12 Octobre 2010

The View of Lithosphere Rheology from Interseismic Deformation : Potential Biases Due to Model Simplification

Overview 1. Continental strength profiles ; a. rock deformation view b. the geodetic view 2. Lessons from the Central Nevada Seismic Belt ; 3. P...

Auteur : Oxburgh E. R., Parmentier E. M., Froidevaux C., ...[et al.] Mercredi 24 Novembre 2010

Thermal processes in the formation of continental lithosphere

Summary Thermal processes in the formation of continental lithosphere ; 1. Introduction, 2. Radioactivity, erosion and cooling, Continental lith...

Auteur : Yegorova T., Yanovskaya T., Gobarenko V., ...[et al.]

Lithosphere structure of the Black Sea basin from seismic tomography and 3D gravity analysis

Black Sea Basin is a back-arc basin formed in the Latest Creataceous (or at the Cretaceous-Palaeo-gene boundary) at the hinterland of the Pontide...

Auteur : Jackson James, McKenzie Dan, Priestley Keith, ...[et al.] Mardi 01 Juin 2010

Earthquake depth distributions in central Asia and lithosphere rheology

This talk will examine the depth distribution of earthquakes in the greater Tibetan region in the context of our current understanding of lithosph...

Abhatoo - Centre Nationale de Documentation

Répartition spatiale des sédiments dans le bassin Ouest-Alboran et sa marge marocaine

Mise en évidence d’une tectonique distensive associée à la convergence Eurasie-Afrique dans le Nord de la Meseta occidental marocaine durant le Plio-Quaternaire

Rôle des transferts multiples de contraintes, déficit de sismicité et caractéristiques physiques des ruptures sismiques

Activité sismique et signal radon: Cas de quelques séismes de magnitude supérieure à 5

Intracontinental Tectonics, Stresses, and Fracture Reservoirs

The Statistical Upper Mantle Assemblage

The role of serpentine in preferential craton formation in the late Archean by lithosphere underthrusting

Does the mantle control the maximum thickness of cratons ?

Mapping the mantle lithosphere for diamond potential using teleseismic methods

Limits of hydrosphere-lithosphere interaction: Origin of the lowestknown δ18O silicate rock on Earth in the Paleoproterozoic Karelian rift

Mantle lithosphere control of crustal tectonics and magmatism of the western Ohře (Eger) Rift

A method of calculating lithosphere thickness from observations of deglacial land uplift and tilt

Consideration of material compressibility in GIA modelling

Distribution and Evolution of Uranium in the Oceanic Lithosphere

Lithosphere delamination with foundering of lower crust and mantle caused permanent subsidence of New Caledonia Trough and transient uplift of Lord Howe Rise during Eocene and Oligocene initiation of Tonga-Kermadec subduction, western Pacific

Isostatic state and density structure from surface to depth of the lithosphere below the Norwegian continental margin

Fractal analysis of subionospheric LF propagation data and consideration of the lithosphere-atmosphere-ionosphere coupling

The View of Lithosphere Rheology from Interseismic Deformation : Potential Biases Due to Model Simplification

Physiography of the Ocean Basins

Thermal processes in the formation of continental lithosphere

Analogue modeling of lithospheric orocline bending. Implications on the development of the Ibero-Armorican Arc

Lithosphere structure of the Black Sea basin from seismic tomography and 3D gravity analysis

Magnetotelluric investigation of the Iberian lithosphere and asthenosphere beneathTajo Basin and Betic Cordillera (PICASSO - Phase I)

Earthquake depth distributions in central Asia and lithosphere rheology

Continental rifting as a function of lithosphere mantle strength

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