The Scandinavian mountains have not persisted since the Caledonian orogeny. A comment on Nielsen et al. (2009a)
- 31 August 2010
- journal article
- research article
- Published by Elsevier BV in Journal of Geodynamics
- Vol. 50 (2), 94-101
- https://doi.org/10.1016/j.jog.2010.02.001
Abstract
No abstract availableThis publication has 44 references indexed in Scilit:
- Neogene inversion of the Central Graben and Ringkøbing-Fyn High, DenmarkTectonophysics, 2009
- Delamination of eclogitized lower crust: Control on the crust–mantle boundary in the central Fennoscandian shieldTectonophysics, 2008
- EuCRUST‐07: A new reference model for the European crustGeophysical Research Letters, 2008
- Structural, Sedimentologic, and Sea-Level Controls on Sand Distribution in a Steep-Clinoform Asymmetric Wave-Influenced Delta: Miocene Billund Sand, Eastern Danish North Sea and JyllandJournal of Sedimentary Research, 2008
- Chalk porosity and sonic velocity versus burial depth: Influence of fluid pressure, hydrocarbons, and mineralogyAAPG Bulletin, 2008
- Exhumation and uplift of the Shillong plateau and its influence on the eastern Himalayas: New constraints from apatite and zircon (U‐Th‐[Sm])/He and apatite fission track analysesTectonics, 2007
- Investigation of multi-phase erosion using reconstructed shale trends based on sonic data. Sole Pit axis, North SeaGlobal and Planetary Change, 2000
- Dynamics of intra-plate compressional deformation: the Alpine foreland and other examplesTectonophysics, 1995
- Meso‐Cenozoic morphotectonic evolution of southern Norway: Neogene domal uplift inferred from apatite fission track thermochronologyTectonics, 1995
- A chemical kinetic model of vitrinite maturation and reflectanceGeochimica et Cosmochimica Acta, 1989