| 1. | The Aleutian Basin is another example of a relatively inactive oceanic basin.
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| 2. | *Ocean drilling is done on the continental shelves, not normally in deep oceanic basins.
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| 3. | Aravalli orogeny ( ~ 1, 800 Ma ) began with the development of oceanic basin.
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| 4. | The elements of an active oceanic basin often include the oceanic trench associated with a subduction zone.
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| 5. | It is tolerant of low dissolved oxygen levels, allowing it to inhabit oceanic basins inaccessible to other sharks.
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| 6. | This area is considered a present-day example of continental rifting leading to seafloor spreading and producing an oceanic basin.
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| 7. | During the Paleoproterozoic Era, the opening of Aravalli oceanic basin separated the eastern Bundelkhand craton and the western Marwar craton.
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| 8. | The Pacific Ocean is also an active, shrinking oceanic basin, even though it has both spreading ridge and oceanic trenches.
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| 9. | This crustal uplift has created extension and horst and grabens and even listric faults which indicate a pre-oceanic basin structure.
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| 10. | The Atlantic ocean and the Arctic ocean are good examples of active, growing oceanic basins, whereas the Mediterranean Sea is shrinking.
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