Experimental Constraints on Hercynian Anatexis in the Iberian Massif, Spain [PDF]
Journal of Petrology, 2000 We have studied experimentally the melting relationships of the Ollo de Sapo gneiss (OSG), an important crustal protolith for the Iberian leucogranites, of possible volcanoclastic origin. The results of this study are compared with previously determined PTt paths, allowing us to interpret the mechanisms of melting and granitoid production during the ...
Castro, A. +5 more
openaire +2 more sources
Radiometric Constraints on the Timing, Tempo, and Effects of Large Igneous Province Emplacement
Geophysical Monograph Series, Page 27-82., 2021 Exploring the links between Large Igneous Provinces and dramatic environmental impact
An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Jennifer Kasbohm +2 more
wiley +1 more source
Geologica Acta, 2022 This work assessed the age distribution of Cadomian/Pan-African orogenic events (550-590 and 605-790Ma, respectively) in several zones of Iberian Massif by means of detrital and inherited zircon analysis compilation. Detrital zircon age spectra show that
Martim Chichorro +4 more
doaj +1 more source
BSGF - Earth Sciences Bulletin, 2022 Rare-element granites and pegmatites represent important sources of raw materials for “clean, green and high technologies”, such as lithium and tantalum, for example.
Melleton Jérémie +5 more
doaj +1 more source
Sociobiology, 2018 A phylogenetic tree of the Iberian Aphaenogaster species - except for A. splendida (Roger) - and a key to the worker caste of all Iberian Aphaenogaster species are proposed. The position of A. striativentris Forel and A.
Kiko Gómez +2 more
doaj +1 more source
Geothermal Energy, 2023 Renewable energy sources are key to achieve the transition toward clean energy system. Among them, the geothermal energy has a production whose effectiveness requires sufficient understanding of the temperature distribution and fluid circulation at depth,
M. Torne +8 more
doaj +1 more source
Strike-slip shear zones of the Iberian Massif: Are they coeval? [PDF]
Lithosphere, 2017 Strike-slip shear zones of the Variscan orogen are used to derive the evolution of paleostrain and discuss the kinematics of the waning stages of the Gondwana-Laurussia collision during the amalgamation of Pangea. In the Iberian Massif, the recognition of three late Carboniferous deformation events related to strike-slip tectonics (D3, D4, D5) in the ...
Rubén Díez Fernández +1 more
openaire +2 more sources
Half-Century Changes in LULC and Fire in Two Iberian Inner Mountain Areas
Fire, 2019 Wildfires in the Iberian Peninsula were large and frequent in the second half of the 20th century. Land use and land cover (LULC) also changed greatly.
Catarina Romão Sequeira +3 more
doaj +1 more source
The Appinite-Migmatite Complex of Sanabria, NW Iberian Massif, Spain [PDF]
Journal of Petrology, 2003 The Sanabria appinitic rocks and host migmatites form an unusual, non-peri-batholithic complex in which all the typical members of the appinite suite are present. It differs from most appinitic complexes in the deeper level of emplacement and the close temporal and spatial association with migmatites.
Castro Dorado, Antonio +6 more
openaire +3 more sources
Glaciers Landscapes during the Pleistocene in Trevinca Massif (Northwest Iberian Peninsula)
Land, 2023 The Trevinca Massif is in the northwestern Iberian Peninsula, on the border between Galicia and Castilla-León. Its highest elevation is 2124 m at the Trevinca peak.
Augusto Pérez-Alberti +1 more
doaj +1 more source