continental margin वाक्य
उदाहरण वाक्य
मोबाइल
- North of this was the Columbia Embayment, where the continental margin was east of the surrounding areas.
- The passive continental margin became active when the Farallon Plate started to dive below the North American Plate.
- At times some of the metamorphosed downgoing slab may be thrust up or obducted onto the continental margin.
- The Stephen Formation formed at a low-latitude miogeoclinic continental margin, at the western limit of a continental craton.
- Due to its increased density, it flows down the Antarctic continental margin and continues north along the bottom.
- Until recently, technological limitations had prevented extensive and detailed mapping of the U . S . continental margin,
- Unlike most subduction zones worldwide, there is no deep oceanic trench present along the continental margin in Cascadia.
- In plate tectonic terms, the Atlantic Plain is known as a classic example of a passive continental margin.
- Another major point of discussion regards the presence of erosional deep canyons along the continental margins of the Basins.
- As plants took hold on the continental margins, oxygen levels increased and carbon dioxide dropped, although much less dramatically.
- Unlike most subduction zones worldwide, no oceanic trench is present along the continental margin in Cascadia earthquake of 1700.
- During Late Carboniferous there was a continental margin with an oceanic trench subducting the ocean floor off the coast.
- Over time, plate tectonics moved this amalgamation of crust generally northeastward into contact with the North American continental margin.
- The other side of the basin is bounded by the Cameroon Volcanic Line and the transform passive continental margin.
- Active continental margins have narrow, relatively steep shelves, due to frequent earthquakes that move sediment to the deep sea.
- While continental margins are typically the most deformed in orogenic events, the interior of continental plates can also deform.
- This implies formation at the continental margin, and then rifting, in the manner of the second class of models.
- Transform faults are not limited to oceanic crust and spreading centers; many transform faults are located on continental margins.
- First, the passive margin stage with orogenic loading of previously stretched continental margin during the early stages of convergence.
- This indicated that there was still insufficient knowledge about transport processes and biological turnover of organic carbon along continental margins.
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