Shear zone vs folding origin for spiral inclusion trails in the Canton Schist
Authors:
- Aaron StallardASAaron Stallard
- Ken HickeyKHKen Hickey
- 1 December 2001
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 23 (12) , 1845-1864
Abstract
No abstract availableKeywords
This publication has 48 references indexed in Scilit:
- Fold mechanisms in the Canton Schist: constraints on the contribution of flexural flowJournal of Structural Geology, 2001
- Porphyroblast inclusion trail geometries in the Grand Canyon: evidence for non-rotation and rotation?Journal of Structural Geology, 2000
- Near-orthogonal foliation development in orogens: meaningless complexity, or reflection of fundamental dynamic processes?Journal of Structural Geology, 1999
- Reversed structures and bounce structures: are they recognizable? Are they real?Journal of Structural Geology, 1999
- Are crenulation cleavage zones mylonites on the microscale?Journal of Structural Geology, 1999
- Experimental investigation of the effects of fluid heterogeneity upon the motion of rigid ellipsoidal inclusions during bulk inhomogeneous shorteningJournal of Structural Geology, 1997
- Porphyroblast non-rotation during crustal extension in the Variscan Lys-Caillaouas Massif, PyreneesJournal of Structural Geology, 1995
- Flow variation in layered rocks subjected to bulk flow of various kinematic vorticities: theory and geological implicationsJournal of Structural Geology, 1994
- The kinematic interpretation of obliquely-transected porphyroblasts: an example from the Trois Seigneurs Massif, FranceJournal of Structural Geology, 1994
- The rotation of garnet porphyroblasts around a single fold, Lukmanier Pass, Central AlpsJournal of Structural Geology, 1992