Buy custom DYNAMIC PROCESSES CONTROLLING DEVELOPMENT OF RIFTED BASINS
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| Topic: |
Science
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| Number of pages / Number of words: |
103 / 28626 |
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Depending on constraints on lateral block movements
crustal separation can be achieved after as little as 9 My and as much as 280 My of rifting activity.
Syn-rift basin subsidence is controlled by the isostatic adjustment of the crust to mechanical stretching of
the lithosphere, its magmatic inflation and thermal attenuation of the mantle-lithosphere...
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The magnitude of post-rift subsidence
is a function of the rift-induced thermal anomaly and crustal density changes, the potential temperature of
the asthenosphere and initial water depths. Intraplate stresses can have an overprinting effect on post-rift
subsidence. Stretching factors derived from post-rift subsidence analyses must be corrected for such effects...
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