foredeep उदाहरण वाक्य

उदाहरण वाक्य

1. The Apennines are slumping away to the northeast into the Po Valley and the Adriatic foredeep; that is, the zone where the Adriatic floor is being subducted under Italy.
2. Palaeocurrent and petrographic data from the sandstone and conglomerate indicate that these rocks were derived from the fold-thrust belt, and deposited within the flexural foredeep of the Himalayan foreland basin (; ).
3. To the west, the Apulia Platform plunges downfaulted underneath the terrigenous sediments of the Apennine foredeep; to the southeast, the Jurassic Early Cretaceous margin lies 20 30 km offshore from the present Apulia coastline.
4. The three different formations exposed along the Mesabi Iron Range were deposited along the leading edge of a foredeep basin & ndash; the Animikie Basin & ndash; which transgressed north over the Archean craton during the Penokean orogeny.
5. Deposits of evaporites accumulated earlier in the nearby Carpathian foredeep during the Middle Miocene, and the adjacent Red Sea Basin ( during the Late Miocene ), and in the whole Mediterranean basin ( during the MSC and the Messinian age ).
6. Also on trend with large existing fields, the exploration targets in the Ponte dei Grilli permit area are gas accumulations trapped in thrusted anticlines, stratigraphic pinch outs and structural features in the Plio-Pleistocene turbiditic sands located in the Apennines foredeep.
7. The plain is the surface of an in-filled system of ancient canyons ( the " Apennine Foredeep " ) extending from the Piave and Tagliamento of the Venetian Plain to the north, among the many streams that empty into the north Adriatic from the west and north.
8. A typical foreland basin is subdivided into a wedge-top basin above the active orogenic wedge, the foredeep immediately beyond the active front, a forebulge high of flexural origin and a back-bulge area beyond, although not all of these are present in all foreland-basin systems.
9. Huge accumulations of sediment that have been fed from Himalayan erosion has been produced due to the deepening of the Bengal Basin, with the thickness of sediment above the Precambrian basement increasing from a few hundred metres in the shelf region to over 18 km in the Bengal foredeep to the south.
10. Compressional forces have been acting from north to south in the Alps and from south to north in the Apennines, but instead of being squeezed into mountains the valley has been subsiding at 1 to per year since about 25 mya, before the Apennines It is now known to be not an erosional feature but is a filled portion of the Adriatic Trench, called the Adriatic foredeep after its function as a subduction zone was discovered.