MadSci Network: Earth Sciences |
The global cycles of relative changes in sea level was published in 1977 by Vail et al., where three orders of cycles were recognized, with duration of - 200-300 million years - 10-80 million years - 1-10 million years These cycles were characterized by slow increases in relative sea level, followed by periods of rapid falls, on timescales of less than 1 million year. The magnitude of these variations is about 1 cm/1000 years, and it can be caused mainly by two factors: - glacial fluctuations in sealevel, that can cause worldwide changes; - horizontal stresses in the lithospheric plates (order of some kbar). To understand the horizontal stresses, remember that if you have a thin rubber, and compresses it horizontally, it will suffer deformation; the same basic idea applies to the plates, although the forces necessary to bend it are much greater. So, these two factors act in the sealevel rise, and in some periods, where there's no evidence of glacial fluctuations, the stresses could be responsible this variation. Eder C. Molina Institute of Astronomy and Geophysics University of Sao Paulo BRAZIL eder@iag.usp.br
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