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 Authors
| 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 |
| Google Analytic Metrics | Metrics page |