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Summary
| Description |
English: Procedure to correct the depth of a sedimentary unit for eustasy and water depth (which equals to calculate the total subsidence relative to a stationary datum) and subsequently to perform a "backstripping", e.g. to take out the effect of sediment loading from the total subsidence and to calculate the amount of tectonic subsidence (i.e. subsidence due to a tectonic driving force) relative to a stationary datum. This procedure is valid in a water-filled basin, where the sediments and the crust are in isostatic equilibrium with the underlying mantle (according to Airy isostasy model) |
| Date | |
| Source | Own work |
| Author | Stefano Patruno |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 09:13, 17 July 2012 | | 2,639 × 2,810 (1.41 MB) | QuinMr |
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