A case of obduction-related high-pressure, low-temperature metamorphism in upper crustal nappes, Arabian continental margin, Oman: P-T paths and kinematic interpretation
- 14 April 2003
- journal article
- Published by Elsevier
- Vol. 151 (1-4) , 363-386
- https://doi.org/10.1016/0040-1951(88)90253-3
Abstract
No abstract availableKeywords
This publication has 51 references indexed in Scilit:
- Kinematics of oceanic thrusting in the Oman ophiolite: model of plate convergencePublished by Elsevier ,2002
- The upper Hawasina nappes in the central Oman Mountains: stratigraphy, palinspastics and sequence of nappe emplacementGeodinamica Acta, 1987
- Influence of deformation on pressure-temperature paths of metamorphismGeology, 1987
- The composition of chlorite as a function of sulfur and oxygen fugacity; an experimental studyAmerican Journal of Science, 1987
- The system CaO-Al2O3-SiO2-H2O: new phase equilibria data, some calculated phase relations, and their petrological applicationsContributions to Mineralogy and Petrology, 1984
- Talc-Phengite: a Widespread Assemblage in High-Grade Pelitic Blueschists of the Western AlpsJournal of Petrology, 1981
- High-pressure-low-temperature metamorphism and polyphase alpine deformation at Sant'Andrea di cotone (eastern corsica, france)Tectonophysics, 1981
- Optical Determination of Topotactic Aragonite-Calcite Growth Kinetics: Metamorphic ImplicationsThe Journal of Geology, 1981
- High fluid pressure, isothermal surfaces, and the initiation of nappe movementGeology, 1980
- Low-temperature compatibility relations of the assemblage quartz-paragonite and the thermodynamic status of the phase rectoriteContributions to Mineralogy and Petrology, 1973