Correlating deformation in Variscan NW-Iberia using porphyroblasts; implications for the Ibero-Armorican Arc
- 1 January 2004
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 26 (1) , 177-196
Abstract
No abstract availableKeywords
This publication has 51 references indexed in Scilit:
- Shear zone vs folding origin for spiral inclusion trails in the Canton SchistJournal of Structural Geology, 2001
- Reading history of folding from porphyroblastsJournal of Structural Geology, 2001
- Partitioning of vorticity in bimineralic rocksJournal of Structural Geology, 2001
- The formation of an orocline by multiphase deformation: a paleomagnetic investigation of the Cantabria–Asturias Arc (northern Spain)Journal of Structural Geology, 2000
- Origin of a large-scale fold nappe in the Montagne Noire, Variscan belt, FranceJournal of Structural Geology, 1999
- Near-orthogonal foliation development in orogens: meaningless complexity, or reflection of fundamental dynamic processes?Journal of Structural Geology, 1999
- Analysis of kilometric-scale superposed folding in the Central Coal Basin (Cantabrian zone, NW Spain)Journal of Structural Geology, 1995
- Porphyroblast non-rotation during crustal extension in the Variscan Lys-Caillaouas Massif, PyreneesJournal of Structural Geology, 1995
- Deformation history of the Otago schists, New Zealand, from progressively developed porphyroblast-matrix microstructures: uplift-collapse orogenesis and its implicationsJournal of Structural Geology, 1990
- A geometrical and kinematical approach to the nappe structure in an arcuate fold belt: the Cantabrian nappes (Hercynian chain, NW Spain)Journal of Structural Geology, 1984