GEODYNAMIQUE INTERNE PDF

Multidisciplinary Approach to Earthquake Prediction pp Cite as. The seismicity along major strike-slip plate boundaries like the San-Andreas or the North Anatolian fault zone is relatively shallow. It is restricted to depths not exceeding 15 or 20 km so that the lower crust and the mantle below it are sheared throughout the lithospheric thickness, say down to about km. This last quantity is not measurable and has to be estimated on the basis of laboratory creep data.

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Multidisciplinary Approach to Earthquake Prediction pp Cite as. The seismicity along major strike-slip plate boundaries like the San-Andreas or the North Anatolian fault zone is relatively shallow. It is restricted to depths not exceeding 15 or 20 km so that the lower crust and the mantle below it are sheared throughout the lithospheric thickness, say down to about km. This last quantity is not measurable and has to be estimated on the basis of laboratory creep data.

This requires the knowledge of the exact temperature within the shear zone. Indeed creep laws are highly temperature sensitive. However, this temperature is likely to be strongly modified by the heat dissipated by the deformation itself. This brief argument illustrates the important feedback between thermal and mechanical quantities within the lithosphere.

These can only be computed by solving doubled thermal and mechanical equations Yuen et al. Unable to display preview. Download preview PDF. Skip to main content. This service is more advanced with JavaScript available.

Advertisement Hide. Authors Authors and affiliations C. Froidevaux L. This is a preview of subscription content, log in to check access. Aki, K. Determination of the three dimensional structure of the lithosphere, J.

Res, 82, — Google Scholar. Cockerham, R. Three-dimensional large-scale mantle structure in central California, EOS, 60, Fleitout, L.

Thermal and mechanical evolution of shear zones, J. Kohlstedt, D. Low-stress high-temperature creep in olivine single crystals, J. Lachenbruch, A. Yuen, C. Shear deformation along major transform faults and sub-ducting slabs, Geophys. Froidevaux 1 L. Fleitout 1 1. Personalised recommendations. Cite chapter How to cite? ENW EndNote. Buy options.

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Tag: Kmz – Géodynamique interne

Tectonic Evolution of the Tethyan Region pp Cite as. New paleomagnetic data have been obtained from middle Miocene to Pliocene sedimentary and volcanic formations in central Aegea, in western Anatolia and in the Antalya basin in southern Anatolia. Together with the previous results obtained in northwestern Greece and with results from northern Aegea reported by other authors they suggest that the lower Miocene arc was originally almost rectilinear and that its curvature has been acquired tectonically most probably by opposed rotational deformations at both terminations. No significant rotation has been measured in the Antalya basin since at least 15 My, confirming that this basin has not been involved in the geodynamic evolution of the Ionian-Lycian arc. Furthermore, the values of inclination obtained from Miocene formations, both sedimentary or volcanic, are systematically shallower than expected for the geocentric dipole field. This suggests that all these regions have undergone a northward drift since middle Miocene. Unable to display preview.

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A Thermal Window in the Lithosphere Underneath North Anatolia and California

National data and global KMZ-en open in temporary locations. They are not registered at closing of the software. KMZ-en files open in temporary locations. In Layers.

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Kmz – Géodynamique interne Géodynamique externe — Google Earth Center

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