Differential loading by prograding sedimentary wedges on continental margins: An arch-forming mechanism

Author:

Kjeldstad A.1,Skogseid J.2,Langtangen H. P.3,Bjørlykke K.4,Høeg K.4

Affiliation:

1. Norske Shell A/S; Tananger Norway

2. Norsk Hydro ASA; EPI; Oslo Norway

3. Simula Research Laboratory; Lysaker Norway

4. Department of Geology; University of Oslo; Oslo Norway

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference57 articles.

1. General theory of three dimensional consolidation;Biot;J. Appl. Phys.,1941

2. Effects of burial diagenesis on stresses, compaction and fluid flow in sedimentary basins;Bjørlykke;Mar. Pet. Geol.,1997

3. Structural evolution of the Vøring Basin, Norway, during the late Cretaceous and Paleogene;Bjørnseth;J. Geol. Soc. London,1997

4. Blystad , P. R. Brekke B. Fraeseth T. Larsen J. Skogseid Structural elements of the Norwegian Continental Shelf; partii: The Norwegian Sea region NPD-Bull. 8, The Norw. Pet. Dir. 1995

5. Geol. Soc. Spec. Publ.;Brekke,2000

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