Shearing within lower crust during progressive retrogression: Structural analysis of gabbroic rocks from the Godzilla Mullion, an oceanic core complex in the Parece Vela backarc basin
Authors:
- Yumiko HariganeYHYumiko Harigane
- Katsuyoshi MichibayashiKMKatsuyoshi Michibayashi
- Yasuhiko OharaYOYasuhiko Ohara
Open Access
- 1 October 2008
- journal article
- research article
- Published by Elsevier in Tectonophysics
- Vol. 457 (3-4) , 183-196
Abstract
No abstract availableKeywords
This publication has 35 references indexed in Scilit:
- Development of lattice preferred orientation in clinoamphiboles deformed under low-pressure metamorphic conditions. A SEM/EBSD study of metabasites from the Aracena metamorphic belt (SW Spain)Journal of Structural Geology, 2007
- Development of shape- and lattice-preferred orientations of amphibole grains during initial cataclastic deformation and subsequent deformation by dissolution–precipitation creep in amphibolites from the Ryoke metamorphic belt, SW JapanJournal of Structural Geology, 2004
- Constraints on deformation conditions and the origin of oceanic detachments: The Mid‐Atlantic Ridge core complex at 15°45′NGeochemistry, Geophysics, Geosystems, 2003
- Deformation and recrystallization of plagioclase along a temperature gradient: an example from the Bergell tonaliteJournal of Structural Geology, 2003
- Dynamic recrystallization processes in plagioclase porphyroclastsJournal of Structural Geology, 2001
- Albite crystallographic preferred orientation and grain misorientation distribution in a low-grade mylonite: implications for granular flowJournal of Structural Geology, 2000
- Origin of extensional core complexes: Evidence from the Mid‐Atlantic Ridge at Atlantis Fracture ZoneJournal of Geophysical Research, 1998
- Abyssal peridotite mylonites: implications for grain-size sensitive flow and strain localization in the oceanic lithosphereTectonophysics, 1996
- Syntectonic development of a strain-independent steady-state grain size during mylonitizationTectonophysics, 1993
- Preferred lattice orientations of plagioclase from amphibolite and greenschist facies rocks near the Insubric Line (Western Alps)Tectonophysics, 1987