Tectonostratigraphic modelling of Cenozoic uplift and erosion in the south-western Barents Sea
- 26 March 2003
- journal article
- Published by Elsevier
- Vol. 11 (4) , 478-490
- https://doi.org/10.1016/0264-8172(94)90081-7
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- Intraplate stresses and dynamical aspects of rifted basinsPublished by Elsevier ,2003
- Stress in the Indo-Australian platePublished by Elsevier ,2003
- Effects of finite rifting times on the development of sedimentary basinsPublished by Elsevier ,2002
- Factors controlling the style of continental rifting: insights from numerical modellingPublished by Elsevier ,2002
- Large uplift of rift flanks: A genetic link with lithospheric rigidity?Earth and Planetary Science Letters, 1992
- Plate reorganization: a cause of rapid late Neogene subsidence and sedimentation around the North Atlantic?Journal of the Geological Society, 1990
- A physical explanation of the relation between flank uplifts and the breakup unconformity at rifted continental marginsGeology, 1989
- Stress fields in the European platform at the time of Africa‐Eurasia collisionTectonics, 1987
- On a tectonic mechanism for regional sealevel variationsEarth and Planetary Science Letters, 1985
- Evolution of passive continental margins and initiation of subduction zonesNature, 1982