Mechanical development of vein structures due to the passage of earthquake waves through poorly-consolidated sediments

Author:

Brothers R.J.,Kemp A.E.S.,Maltman A.J.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference33 articles.

1. Initial tectonic deformation of hemipelagic sediment at the leading edge of the Japan convergent margin;Arthur,1980

2. Evolution of structures and fabrics in the Barbados Accretionary Prism;Behrmann;J. Struct. Geol.,1988

3. The Mechanical Development of Vein Structures as Fluid Pathways in Diatomaceous Sediments from the Peru Margin and Monetery Formation, California;Brothers,1995

4. An Introduction to the Theory of Seismology;Bullen,1965

5. Structural features in Leg 128 cores: Relationships with the tectonic evolution of the Japan Sea;Charvet,1992

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