oceanic basin वाक्य
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- The Aleutian Basin is another example of a relatively inactive oceanic basin.
- *Ocean drilling is done on the continental shelves, not normally in deep oceanic basins.
- Aravalli orogeny ( ~ 1, 800 Ma ) began with the development of oceanic basin.
- The elements of an active oceanic basin often include the oceanic trench associated with a subduction zone.
- It is tolerant of low dissolved oxygen levels, allowing it to inhabit oceanic basins inaccessible to other sharks.
- This area is considered a present-day example of continental rifting leading to seafloor spreading and producing an oceanic basin.
- During the Paleoproterozoic Era, the opening of Aravalli oceanic basin separated the eastern Bundelkhand craton and the western Marwar craton.
- The Pacific Ocean is also an active, shrinking oceanic basin, even though it has both spreading ridge and oceanic trenches.
- This crustal uplift has created extension and horst and grabens and even listric faults which indicate a pre-oceanic basin structure.
- The Atlantic ocean and the Arctic ocean are good examples of active, growing oceanic basins, whereas the Mediterranean Sea is shrinking.
- One of the largest LIPs in the world, the Kerguelen Plateau covers an area of and rises above the surrounding oceanic basins.
- Anaerobic digestion occurs naturally in some soils and in lake and oceanic basin sediments, where it is usually referred to as " anaerobic activity ".
- The elements of an active-and growing-oceanic basin include an elevated mid-ocean ridge, flanking abyssal hills leading down to abyssal plains.
- The species " Hippasteria phrygiana " may be one of the most widely distributed species : it is present in the 3 main oceanic basins.
- Perhaps the best example of an inactive oceanic basin is the Gulf of Mexico, which formed in Jurassic times and has been doing nothing but collecting sediments since then.
- Liquid water was prevalent, and deep oceanic basins are known to have existed attested by the presence of banded iron formations, chert beds, chemical sediments and pillow basalts.
- Since the new oceanic basins are shallower than the old oceanic basins, the total capacity of the world's ocean basins decreases during times of active sea floor spreading.
- Since the new oceanic basins are shallower than the old oceanic basins, the total capacity of the world's ocean basins decreases during times of active sea floor spreading.
- Geologically, an oceanic basin may be actively changing size or may be relatively, tectonically inactive, depending on whether there is a moving plate tectonic boundary associated with it.
- This system has a global domain of approximately 50 km resolution, with nested regional domains for the northern hemisphere oceanic basins at approximately 18 km and approximately 7 km resolution.
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