alpine orogeny वाक्य
उदाहरण वाक्य
मोबाइल
- The northward movement of the African Plate and its collision with the European Plate then caused the Alpine Orogeny, beginning in the late Mesozoic.
- The Alpine orogeny was the main cause of extensive tectonic activities and it was responsible for the formation of the hydrothermal field within the region.
- During the Palaeogene the south-east of England was affected by movements related to the formation of the Alps ( the Alpine Orogeny ).
- At this time, the Alpine Orogeny, the major mountain building event that was to produce the Alps, was in its early stages.
- The Alpine Orogeny that occurred about 50 Ma was responsible for the shaping of the London Basin syncline and the Weald anticline to the south.
- The Paratethys was separated from the Tethys by the formation of the Alps, Carpathians, Dinarides, Taurus and Elburz mountains during the Alpine orogeny.
- The massif arose during the Alpine orogeny, when the African, Indian and Cimmerian Plates, and smaller Asian terranes, collided with that of Eurasia.
- The uplift of the horst-like fault block was part of the Saxonian tectonic processes and is understood as a long range effect of the Alpine orogeny.
- The Alpine Orogeny that took place about 50 million years ago was responsible for the shaping of the London Basin syncline and the Weald anticline to the south.
- In general the Massif Central is an asymmetric basement plate elevated at its southern margin by the Pyrenees orogeny and along its eastern margin by the Alpine orogeny.
- In the Eocene and early Oligocene, the Adriatic Plate moved north and north-east, contributing to the Alpine orogeny via the tectonic uplift of the Dinarides.
- The Alpine orogeny occurred in ongoing cycles through to the Paleogene causing differences in nappe structures, with a late-stage orogeny causing the development of the Jura Mountains.
- Another important element of Austrian geology and geography is the late Mesozoic Alpine orogeny, and the subsequent formation of the Paratethys ocean and Molasse Basin in the Cretaceous era.
- These fractures lie along the structural axes of the island itself, forming themselves from the Alpine orogeny during the Tertiary Period due to the movements of the African plate.
- The Rhine flows from the Alps to the North Sea Basin; the geography and geology of its present-day watershed has been developing, since the Alpine orogeny began.
- In between the zone of Alpine orogeny and North Sea Basin subsidence, remained highlands resulting from an earlier orogeny ( Variscan ), such as the Ardennes, Eifel and Vosges.
- Due to geological folding of the Alpine orogeny, the strata in the main section of the bay are near vertical, with younger rocks with progressively lower dips to the west.
- In the Upper Cretaceous area of Tatric Unit, was affected by Eo-Alpine of Alpine Orogeny, that caused movement of large masses of rocks to the North and Northeast.
- They represent the inner continental shelf on the southern edge of pre-Alpine Europe and they were not affected by the folding and overthrusting processes of the Alpine Orogeny until relatively late.
- During the late stages of the Alpine Orogeny, as the African Plate collided with Eurasian Plate, Mesozoic extensional structures, such as the Weald Basin of southern England, underwent structural inversion.
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