The 3D interplay between folding and faulting in a syn-orogenic extensional system: the Simplon Fault Zone in the Central Alps (Switzerland and Italy)-Reference-Cited by-同舟云学术

The 3D interplay between folding and faulting in a syn-orogenic extensional system: the Simplon Fault Zone in the Central Alps (Switzerland and Italy)

Published:2014-08-23 Issue:2-3 Volume:107 Page:251-271
ISSN:1661-8726
Container-title:Swiss Journal of Geosciences
language:en
Short-container-title:Swiss J Geosci

Author:

Campani Marion,Mancktelow Neil,Courrioux Gabriel

Publisher

Springer Science and Business Media LLC

Subject

Geology

Link

http://link.springer.com/content/pdf/10.1007/s00015-014-0163-y.pdf

Reference57 articles.

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2. Avigad, D., Ziv, A., & Garfunkel, Z. (2001). Ductile and brittle shortening, extension-parallel folds and maintenance of crustal thickness in the central Aegean (Cyclades, Greece). Tectonics, 20, 277–287.

3. Axen, G. J., Selverstone, J., & Wawrzyniec, T. (2001). High-temperature embrittlement of extensional Alpine mylonite zones in the midcrustal ductile-brittle transition. Journal of Geophysical Research-Solid Earth, 106, 4337–4348.

4. Bartley, J. M., Fletcher, J. M., & Glazner, A. F. (1990). Tertiary extension and contraction of lower-plate rocks in the Central Mojave metamorphic core complex, Southern California. Tectonics, 9, 521–534.

5. Buck, W. R. (1988). Flexural rotation of normal faults. Tectonics, 7, 959–973.

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