The lithosphere is subject to fluctuations in temperature and pressure during the formation of sedimentary basins. These fluctuations cause metamorphic reactions that change the density of the lithosphere, which, in turn, influences basin subsidence. This contribution develops a model for sedimentar
Rheology of the Earth and a thermoconvective mechanism for sedimentary basin formation
✍ Scribed by Boris I. Birger
- Book ID
- 104460757
- Publisher
- John Wiley and Sons
- Year
- 1998
- Tongue
- English
- Weight
- 312 KB
- Volume
- 134
- Category
- Article
- ISSN
- 0956-540X
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