J
J. R. Martínez Catalán
Researcher at University of Salamanca
Publications - 37
Citations - 1664
J. R. Martínez Catalán is an academic researcher from University of Salamanca. The author has contributed to research in topics: Massif & Shear zone. The author has an hindex of 20, co-authored 37 publications receiving 1544 citations.
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Journal ArticleDOI
Diachronous Variscan tectonothermal activity in the NW Iberian Massif: Evidence from 40Ar/39Ar dating of regional fabrics
R.D. Dallmeyer,J. R. Martínez Catalán,Ricardo Arenas,J.I. Gil Ibarguchi,Gabriel Gutiérrez Alonso,P. Farias,Fernando Bastida,Jesús Aller +7 more
TL;DR: In this article, multigrain concentrates of hornblende and muscovite together with whole-rock slate/phyllite samples have been dated using 40Ar/39Ar incremental-release methods along a systematic traverse across the various lithotectonic structural elements which comprise northwestern sectors of the Variscan Iberian Massif.
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Early Ordovician orogenic event in Galicia (NW Spain): evidence from U–Pb ages in the uppermost unit of the Ordenes Complex
Jacobo Abati,G. R. Dunning,Ricardo Arenas,F. Díaz García,P. González Cuadra,J. R. Martínez Catalán,Pilar Andonaegui +6 more
TL;DR: In this article, the uppermost allochthon in the Variscan belt of NW Spain has been studied and it is shown that the hangingwall to the suture includes a pre-Variscan tectonothermal unit.
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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 decompression
TL;DR: The Santiago Schists are located in the Basal Unit of the Ordenes Complex, one of the allochthonous complexes outcropping in the inner part of the Hercynian Belt in the north-west of the Iberian Peninsula.
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U-Pb zircon and monazite geochronology of Variscan magmatism related to syn-convergence extension in Central Northern Portugal
TL;DR: In this article, the authors reported high precision U-Pb zircon and monazite ages for four plutons of the Viseu area: the syn-kinematic granitoids of Maceira (314±5 Ma), Casal Vasco (311±1 Ma), Junqueira (307.8±0.7 Ma), and Cota (306±9 Ma).
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Role of the Ollo de Sapo massive felsic volcanism of NW Iberia in the Early Ordovician dynamics of northern Gondwana
TL;DR: The Ollo de Sapo Fm. as mentioned in this paper is made up of two large superposed volcanic domes separated by a thin screen of contemporaneous metapelites and sandstones.