Buckling of the oceanic lithosphere from geophysical data and experiments
Two major hypothesis have been advanced for the formation of the long wavelength (100-300) km undulations of oceanic basement and overlying sediments developed in the central Indian Ocean: whole layer folding (buckling) and local thickening (inverse boudinage). Using appropriately scaled two layer m...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
1992-06.
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Subjects: | |
Online Access: | Get fulltext |