Compaction of basin sediments: modeling based on time-temperature history
Journal of Geophysical Research
- By:
- J.W. Schmoker and D.L. Gautier
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Abstract
Dependence of porosity upon integrated time-temperature history implies that basin sediments are not in equilibrium but compact through geologic time. Calculations show that subsidence resulting from the loss of porosity with increasing time-temperature exposure (as opposed to deeper burial) can produce a second-stage, passively formed basin containing many hundreds of meters of sediments. -from AuthorsAdditional publication details
- Publication type:
- Article
- Publication Subtype:
- Journal Article
- Title:
- Compaction of basin sediments: modeling based on time-temperature history
- Series title:
- Journal of Geophysical Research
- Volume:
- 94
- Issue:
- B6
- Year Published:
- 1989
- Language:
- English
- Larger Work Type:
- Article
- Larger Work Subtype:
- Journal Article
- Larger Work Title:
- Journal of Geophysical Research
- First page:
- 7379
- Last page:
- 7386