Significance of dextral reactivation of an E-W transfer fault in the formation of the Pennsylvania orocline, central Appalachians-Reference-Cited by-同舟云学术

Significance of dextral reactivation of an E-W transfer fault in the formation of the Pennsylvania orocline, central Appalachians

Published:2004-10 Issue:5 Volume:23 Page:n/a-n/a
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Yeh M.-W.,Bell T. H.¹

Affiliation:

1. School of Earth Sciences; James Cook University; Townsville, Queensland; Australia

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference88 articles.

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2. The Covington-Clifton Forge Fault: More evidence for post-folding rotation of the southern Appalachians (abstract);Alterman;Geol. Soc. Am. Abstr. Programs,1983

3. The orocline hypothesis versus thin skin rotation in the central and southern Appalachians;Alterman;Geophys. Res. Lett.,1984

4. Foliation development: The contribution, geometry and significance of progressive bulk inhomogeneous shortening;Bell;Tectonophysics,1981

5. The development of spiral-shaped inclusion trails during multiple metamorphism and folding;Bell;J. Metamorph. Geol.,2002

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