Small-scale faulting as an indicator of deformation mechanism in the tertiary sediments of the northern Danish Central Trough-Reference-Cited by-同舟云学术

Small-scale faulting as an indicator of deformation mechanism in the tertiary sediments of the northern Danish Central Trough

Published:1993-11 Issue:11 Volume:15 Page:1343-1357
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Clausen Ole Rønø,Korstgåd John A.

Publisher

Elsevier BV

Subject

Geology

Reference38 articles.

1. Compressibility; elastic constants;Birch,1966

2. Transverse structural zones in continental rifts—an example from the Danish sector of the North Sea;Cartwright,1987

3. A method for estimation of the density of fault displacements below the limits of seismic resolution in reservoir formation;Childs,1990

4. Tertiary seismic, stratigraphic and structural evolution of the northern Danish Central Trough;Clausen,1991

5. A possible mechanism relating progradation, growth faulting, clay diapirism and overthrusting in a regressive sequence of sediments;Dailly;Bull. Can. Petrol. Geol.,1976

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