Titlebook: Geological Evolution of the Mediterranean Basin; Raimondo Selli Comme Daniel Jean Stanley,Forese-Carlo Wezel Book 1985 Springer-Verlag New

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Geological Information from Satellite Surveys of the Mediterranean Regioned on satellite images illustrate the existence of all classes of brittle fractures in the upper crust. Lineament patterns suggest the tectonic patterns for a given region, but it is necessary to “field check” any area for which lineament maps are prepared. It is critical that such studies be carrie

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Seismicity of the Mediterranean Basinbetween the African and Eurasian plates. This boundary is of a complex nature, and its dynamics are the consequence of the opening of the Atlantic Ocean and the closing of the Mediterranean Sea. Main tectonic features are of compressive character, with only very localized zones undergoing horizontal

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Some Boundary Conditions for the Evolution of the Mediterranean RegionGondwanaland. The relative motions of stable Africa relative to stable Europe, and vice versa, have been calculated from recently available data. The motions have been shown as increments and as total displacements. The total displacements have also been calculated for the hotspots frame both for st

Cpr951

Cpr951

Tectonic Evolution of the Tyrrhenian Searoplates from the Upper Cretaceous to the middle Pliocene. During this time span the Tyrrhenian Alps and Apennines were formed. From the Tortonian until the present a process of oceanization by mantle diapirism took place in the Tyrrhenian area associated with an extensional tectonic regime oriented

变形词

Structural Features and Basin Tectonics of the Tyrrhenian Sea Its bilateral symmetry, which gives it the character of an interarc basin, is also manifested by the deep crustal configuration that should indicate opposite-vergent arcuate overthrusting (obduction) of the Tyrrhenian oceanic crust onto the Alpine (modern inactive front) and the Apennine (active fr

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Recent Geological Evolution of the Adriatic Seae correlated with those on land. For example, the Sabbie di Asti Formation extends offshore from the Po Valley into the Adriatic Basin to the region immediately east of Ancona. Southward, the equivalent unit is the Sabbie di Carassai Formation, composed of basinal turbidites. In the southwestern par

旧石器时代

Structure and Evolution of the Central Mediterranean (Pelagian and Ionian Seas)riassic, produced continental rifting with prominent effects in the Streppenosa Trough (Sicily-Malta platform area) and in the Ionian Sea. A second extensional phase occurred in the Middle Jurassic and opened the Ionian Sea and Eastern Mediterranean. The Pelagian Sea and Sirte Rise (excluding the up