The blanketing effect of sediments in basins formed by extension: a numerical model. Application to the Gulf of Lion and Viking graben
- 28 October 2002
- journal article
- Published by Elsevier
- Vol. 74 (1) , 92-102
- https://doi.org/10.1016/0012-821x(85)90169-4
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- The variation of temperature with time and hydrocarbon maturation in sedimentary basins formed by extensionPublished by Elsevier ,2002
- The Gulf of Lion: subsidence of a young continental marginNature, 1980
- Continental stretching: An explanation of the Post‐Mid‐Cretaceous subsidence of the central North Sea BasinJournal of Geophysical Research, 1980
- A model of intracratonic basin formation, entailing deep crustal metamorphismGeophysical Journal International, 1980
- Sedimentary basin formation with finite extension ratesEarth and Planetary Science Letters, 1980
- Some remarks on the development of sedimentary basinsEarth and Planetary Science Letters, 1978
- On the thermal and subsidence history of sedimentary basinsJournal of Geophysical Research, 1977
- Thermal and mechanical evolution of the Michigan BasinTectonophysics, 1976
- Thermal conductivity of Earth materials at high temperaturesJournal of Geophysical Research, 1972
- Thermal Effects of the Formation of Atlantic Continental Margins by Continental Break upGeophysical Journal International, 1971