Results 151 to 160 of about 592 (175)
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1984
The most outstanding feature of the Iberian Peninsula is the vast remnant of the Hercynian continent, variously called the Hesperic massif by Hernandez-Pacheco (1932a), the Iberian massif by Lautensach and Mayer (1961) or the Meseta block by Sole-Sabaris (1952): This last term is not to be confused with the physiographic term used for the Castilian ...
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The most outstanding feature of the Iberian Peninsula is the vast remnant of the Hercynian continent, variously called the Hesperic massif by Hernandez-Pacheco (1932a), the Iberian massif by Lautensach and Mayer (1961) or the Meseta block by Sole-Sabaris (1952): This last term is not to be confused with the physiographic term used for the Castilian ...
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Block Streams in the Tremedal Massif, Central Iberian Chain
2014The Tremedal Massif is an inlier of Paleozoic rocks that protrudes around 300 m over an extensive planation surface cut across Mesozoic formations. It reaches 1,920 m a.s.l. at Caimodorro and has a continental climate characterised by a large number of days with minimum temperatures below freezing point (80–100 days per year).
Mateo Gutiérrez, Francisco Gutiérrez
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2023
The Iberian Massif presents a complex Late Paleozoic evolution, with intense compressional tectonics followed by gravitational collapse of the thickened crust and orocline development. In NW Iberia, extensional detachments and associated shear zones developed during high temperature-low pressure metamorphism in relation to partial melting in gneiss ...
Irene Pérez Cáceres +9 more
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The Iberian Massif presents a complex Late Paleozoic evolution, with intense compressional tectonics followed by gravitational collapse of the thickened crust and orocline development. In NW Iberia, extensional detachments and associated shear zones developed during high temperature-low pressure metamorphism in relation to partial melting in gneiss ...
Irene Pérez Cáceres +9 more
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Terranes within the Iberian Massif: Correlations with West African Sequences
1991The Iberian Peninsula consists of two very different parts: (1) the eastern half which constitutes the westernmost extension of the Alpine orogen; and (2) the western half (Iberian Massif) representing the southwesternmost and largest piece of the so-called European Hercynian Foldbelt. Although Precambrian and Paleozoic inliers are scattered within the
C. Quesada +8 more
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2017
A well preserved Cadomian basement is exposed in the Iberian Massif, Central Portugal, at the Ossa Morena/Central Iberian zone boundary, which allows the determination of reliable geochemical data. A sequence of Cadomian and Variscan magmatic and tectonometamorphic events has been already described for this area and are documented in other areas of the
Henriques, S.B.A. +3 more
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A well preserved Cadomian basement is exposed in the Iberian Massif, Central Portugal, at the Ossa Morena/Central Iberian zone boundary, which allows the determination of reliable geochemical data. A sequence of Cadomian and Variscan magmatic and tectonometamorphic events has been already described for this area and are documented in other areas of the
Henriques, S.B.A. +3 more
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Iberian Meseta and the Iberian Massif
Zeitschrift für Geomorphologie, 1961H. Lautensach., E Mayer.
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2022
In the Iberian Massif a voluminous igneous activity was recorded along its reputed rifting axial (i.e., the Ossa-Morena Zone, OMZ) where three phases, separated by relatively quiescent periods, are distinguished. The first two, Early and Main rift-stage magmatic events, were defined in detail by Sánchez García et al.
Chichorro, Martim +5 more
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In the Iberian Massif a voluminous igneous activity was recorded along its reputed rifting axial (i.e., the Ossa-Morena Zone, OMZ) where three phases, separated by relatively quiescent periods, are distinguished. The first two, Early and Main rift-stage magmatic events, were defined in detail by Sánchez García et al.
Chichorro, Martim +5 more
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Lithos, 2003
Abstract Basic rocks included in the Ossa–Morena/Central Iberian Variscan suture of SW Iberia have been studied in order to decipher the pre-orogenic evolution along this major boundary. These rocks appear as garnet-free amphibolites and garnet-bearing amphibolites.
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Abstract Basic rocks included in the Ossa–Morena/Central Iberian Variscan suture of SW Iberia have been studied in order to decipher the pre-orogenic evolution along this major boundary. These rocks appear as garnet-free amphibolites and garnet-bearing amphibolites.
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First orthothecid hyolith from the Ordovician of the Iberian Massif, Spain
Bollettino della Società Paleontologica Italiana, 2022Gutiérrez-Marco, Juan Carlos +1 more
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Silurian conodonts of the Obejo-Valsequillo Domain (SW of the Iberian Massif)
2019Peer ...
Aragonés-Illanas, Pau +2 more
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