Titlebook: Recent Evolution and Seismicity of the Mediterranean Region; E. Boschi,E. Mantovani,A. Morelli Book 1993 Springer Science+Business Media D

TATE

Tyrrhenian Basin and Apennines. Kinematic Evolution and Related Dynamic Constraints,rative study of tectonically- controlled sedimentary sequences and of coeval tectonic features in areas experiencing stretching (Algero-Provençal Basin, Tyrrhenian Basin) and shortening (Apennines). The derived step by step palinspastic reconstruction at Langhian times states a number of constraints

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Neogene Basins in the Strait of Sicily (Central Mediterranean): Tectonic Settings and Geodynamic Imdimentary fill, while in the others the filling is Plio-Quaternary. Tortonian basins are the Adventure foredeep and some narrow grabens, trending NE-SW, present in the foreland. Afterwards, the foredeep was incorporated into the fold-and-thrust belt and the grabens were inverted. Plio-Quaternary bas

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调整

The Determination of Earthquake Size and Source Geometry in the Mediterranean Sea,e discuss applications and limitations of the principal parameters used in quantifying earthquakes: magnitude, fault plane solutions and moment tensors. We present a method for the rapid determination of the moment tensor using digital waveforms from a regional network, suitable for application to r

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,A Review of the Eastern Alps — Northern Dinarides Seismotectonics,on. The present-day seismicity, which is well documented because of the presence of a regional seismometric network, was of particular importance. The seismic area is the pre-Alpine belt which continues eastwards along the Croatian coast; it is delimited southwards by the presently active Alpine and

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Regional Stresses in the Mediterranean Region Derived from Focal Mechanisms of Earthquakes,he Mediterranean basin is located at the plate boundary between the Eurasian and African plates. This boundary is of a complex nature and its dynamics is related to the opening of the Atlantic ocean and the closing of the Thetys sea. From Azores to Gibraltar the motion changes from strike-slip to re

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Source Process of Some Large Earthquakes in Greece and its Tectonic Implication,rriers on the fault plane. The source process has been revealed by the inversion of teleseismic long period body waves using two different techniques. Based on the obtained source time functions an attempt is made to explain the low stress drop values for the earthquakes occurred in Greece. It seems

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P-Wave Teleseismic Tomography: Contribution to the Delineation of the Upper Mantle Structure of Ita tectonic evolution in regions of plate margins. We applied a well established and robust inversion technique (“ACH” technique) to compute a three-dimensional model of the compressional wave velocity in the lithosphere-asthenosphere system beneath Italy. We used a high quality dataset of about 4700