P-T evolution of eclogites from the Agualada Unit (Ordenes Complex, northwest Iberian Massif, Spain): Implications for crustal subduction
- 31 July 1997
- journal article
- Published by Elsevier BV in Lithos
- Vol. 40 (2-4), 221-242
- https://doi.org/10.1016/s0024-4937(97)00029-7
Abstract
No abstract availableKeywords
This publication has 40 references indexed in Scilit:
- High‐pressure micro‐inclusions and development of an inverted metamorphic gradient in the Santiago Schists (Ordenes Complex, NW Iberian Massif, Spain): evidence of subduction and syncollisional decompressionJournal of Metamorphic Geology, 1995
- Polyphase Variscan emplacement of exotic terranes (Morais and Bragança Massifs) onto Iberian successions: Evidence from 40Ar/39Ar mineral agesLithos, 1991
- Age of amphibolitic metamorphism in the ophiolitic unit of the Morais allochthon (Portugal): implications for early Hercynian orogenesis in the Iberian MassifJournal of the Geological Society, 1990
- The stacking of thrust slices in collision zones and its thermal consequencesTectonics, 1986
- A Barometer for Garnet Amphibolites and Garnet GranulitesJournal of Petrology, 1986
- Shear deformation and eclogite formation within granulite-facies anorthosites of the Bergen Arcs, western NorwayChemical Geology, 1985
- Coesite and pure pyrope in high-grade blueschists of the Western Alps: a first record and some consequencesBeiträge zur Mineralogie und Petrographie, 1984
- An experimental study of the effect of Ca upon garnet-clinopyroxene Fe-Mg exchange equilibriaBeiträge zur Mineralogie und Petrographie, 1979
- Isotopic dating of older elements (including the Cabo Ortegal mafic-ultramafic complex) in the Hercynian orogen of NW Spain: Manifestations of a presumed Early Paleozoic mantle-plumeChemical Geology, 1979
- Eclogites and Eclogites: Their Differences and SimilaritiesGSA Bulletin, 1965