Continental Stretching--Explanation of Post-Mid-Cretaceous Subsidence of Central North Sea Basin¶
Sclater, J. G., & Christie, P. A. F. (1980). Continental Stretching--Explanation of Post-Mid-Cretaceous Subsidence of Central North Sea Basin: ABSTRACT. AAPG Bulletin, 50-100.
Cited by¶
1 citation across 1 artifact.
Domain-specific¶
- Rift Zone
- McKenzie's 1978 model let geologists assign a β-factor to that stretching and predict two subsidence phases: rapid syn-rift, fault-controlled subsidence, then slow post-rift thermal-sag subsidence as the heated lithosphere cooled and contracted over tens of millions of years
Supported in partVerified against the publisher's abstract
“A geologic model based on stretching which can account for the Jurassic and Early Cretaceous faulting and the general post-mid-Cretaceous saucer-shaped basin is presented.”
- McKenzie's 1978 model let geologists assign a β-factor to that stretching and predict two subsidence phases: rapid syn-rift, fault-controlled subsidence, then slow post-rift thermal-sag subsidence as the heated lithosphere cooled and contracted over tens of millions of years
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