The Dent Fault System, northern England—reinterpreted as a major oblique-slip fault zone

Author:

UNDERHILL J. R.,GAYER R. A.,WOODCOCK N. H.,DONNELLY R.,JOLLEY E. J.,STIMPSON I. G.

Publisher

Geological Society of London

Subject

Geology

Reference69 articles.

1. Late Paleozoic strike-slip faulting in southern Europe and northern Africa: Result of a right-lateral shear zone between the Appalachians and the Urals

2. The Ribblesdale fold belt, NW England—a Dinantian-early Namurian dextral shear zone;Arthurton,1984

3. Arthurton, R. S. & Wadge A.J. 1981Geology of the country around Penrith. Memoir of the Geological Society of Great Britain, Sheet 24.

4. Strike-slip orogens—an explanation for the Hercynides

5. Tool-Using and Aimed Throwing in a Community of Free-Living Chimpanzees

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