The role of deformation in the formation of metamorphic gradients: Ridge subduction beneath the Oman Ophiolite
- 1 April 1991
- journal article
- Published by American Geophysical Union (AGU) in Tectonics
- Vol. 10 (2), 455-473
- https://doi.org/10.1029/90tc02779
Abstract
No abstract availableThis publication has 64 references indexed in Scilit:
- Grain growth kinetics in olivine aggregatesTectonophysics, 1989
- KAr and Ar study of metamorphic rocks associated with the Oman ophiolite: Tectonic implicationsTectonophysics, 1988
- The Hawasina Basin: A fragment of a starved passive continental margin, thrust over the Arabian Platform during obduction of the Sumail NappeTectonophysics, 1988
- Paleomagnetic results from Oman ophiolites related to their emplacementTectonophysics, 1988
- Shear zones, thrusts and related magmatism in the Oman ophiolite: Initiation of thrusting on an oceanic ridgeTectonophysics, 1988
- The death of an accretion zone as evidenced by the magmatic history of the Sumail ophiolite (Oman)Tectonophysics, 1988
- Structural mapping in the Oman ophiolites: Mantle diapirism along an oceanic ridgeTectonophysics, 1988
- Structure and sequence of thrusting in deep-water sediments during ophiolite emplacement in the south-central Oman MountainsJournal of Structural Geology, 1988
- Geochronology of ophiolites of the Newfoundland AppalachiansCanadian Journal of Earth Sciences, 1985
- Genesis of the Batinah mélange above the Semail ophiolite, OmanJournal of Structural Geology, 1983