Rapid mantle-driven uplift along the Angolan margin in the late Quaternary
Mantle flow can cause the Earth’s surface to uplift and subside, but the rates and durations of these motions are, in general, poorly resolved due to the difficulties in making measurements of relatively small vertical movements (hundreds of metres) over sufficiently large distances (about 1,000 km)...
| Main Authors: | , , , , , , , |
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| Format: | Journal article |
| Izdano: |
Nature Publishing Group
2016
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