Foreland Basins: Lithospheric Flexure, Plate Strength and Regional Stratigraphy
Foreland basin subsidence through time is reproduced in this study, as the flexure of an elastic beam in an inviscid fluid under the vertical stress, caused by discrete-distributed loads. Thus, seismostratigraphic data from the Timor Sea peripheral foreland basin, in northwestern Australia, and the...
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| Format: | Others |
| Language: | en |
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LSU
2004
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| Online Access: | http://etd.lsu.edu/docs/available/etd-05202004-160106/ |