José M. Fuenlabrada- RationaleControl over accuracy and precision in isotope geochemical analysis is highly necessary for reliable results. Use of … Más
Etiqueta: Fuenlabrada Pérez-J. M.
Origin and evolution of Cadomian magmatism in SW Iberia: from subduction onset and arc building to a tectonic switching
Esther Rojo-Pérez (et al.)- The evolution of the Gondwana along the flank of the West African Craton was complex and … Más
Geochemistry of metasedimentary rocks from the Eastern Pyrenees (Iberian Peninsula): Implications for correlation of Ediacaran terranes along the Gondwanan margin
E. Rojo-Pérez (et al.)- The North African margin of Gondwana formed by subduction and accretion during Ediacaran to Cambrian times. … Más
Variability in the sources of North Gondwana Cadomian basins tracked by Nd isotopic systematics (Iberian Massif)
José Manuel Fuenlabrada (et al.)- The Cadomian Orogeny encompassed the opening and closure of oceanic domains and associated sedimentary basins … Más
Cadomian arc recycling along the northern Gondwana margin: Source-inherited composition of Miaolingian rift-related rhyolitic rocks (Ossa-Morena Zone, SW Iberia)
M. F. Pereira (et al.)- Rhyolites and rhyolitic tuffs of the Freixo-Segóvia Volcanic-Sedimentary Complex of the Cambrian of the Ossa-Morena … Más
Opening and closure of Cadomian peri-Gondwanan oceans: age and evolution of the Mérida Ophiolite (SW Iberia)
R. Arenas (et al.)- In the SW Iberian Massif, the Ossa-Morena Complex contains a stack of units of different origin … Más
Changing Carboniferous Arc Magmatism in the Ossa-Morena Zone (Southwest Iberia): Implications for the Variscan Belt
Manuel Francisco Pereira (et al.)- Carboniferous magmatism in southwestern Iberia was continuously active for more than 60 m.y. during the … Más
U-Pb geochronology and isotopic geochemistry of adakites and related magmas in the Ediacaran arc section of the SW Iberian Massif: The role of subduction erosion cycles in peri-Gondwanan arcs
Esther Rojo-Pérez (et al.)- In the peri-Gondwanan Ediacaran arc section outcropping in the SW of the Iberian Massif (Mérida region), … Más
Whole-rock and Sm–Nd isotopic geochemistry of Triassic SW Iberia sandstones: implications for provenance
Cristina Gama (et al.)- Whole-rock and Sm–Nd isotopic geochemistry data were used to characterise the probable sources of the Triassic … Más
Age and petrogenesis of the beryl-bearing granitic magmatism of the Velasco Pegmatite District, Pampeana Province, NW Argentina
Two porphyritic granitoids (Huaco and Sanagasta) in the Velasco district of the Pampeana Pegmatite Province in Northwestern Argentina are recognized. … Más
Tectonostratigraphy of the Mérida Massif reveals a new Cadomian suture zone exposure in Gondwana (SW Iberia)
Rubén Díez Fernández (et al.)- Neoproterozoic and Palaeozoic rocks of the Mérida Massif (SW Iberia) have been grouped into tectonostratigraphic … Más
Geochemistry and Sm–Nd isotopic sources of Late Ediacaran siliciclastic series in the Ossa–Morena Complex: Iberian–Bohemian correlations
Esther Rojo-Pérez (et al.)- The Cadomian basement in central and southern Europe is composed by Ediacaran–Early Cambrian sequences that appear … Más
Tectonic setting and isotopic sources (Sm–Nd) of the SW Iberian Autochthon (Variscan Orogen)
José Manuel Fuenlabrada (et al.)- Metasedimentary rock successions in Sierra Albarrana Group (SW Iberia Autochthonous Domain) were deposited during the … Más
Geochemistry in earth sciences: a brief overview
Javier Fernández-Suárez, Sonia Sánchez Martínez, José M. Fuenlabrada- In this contribution we present a succinct overview of the role of Geochemistry … Más
A unique blueschist facies metapelite with Mg-rich chloritoid from the Badajoz-Córdoba Unit (SW Iberian Massif): correlation of Late Devonian high-pressure belts along the Variscan Orogen
R. Arenas (et al.)- The Badajoz-Córdoba Unit (BCU, SW Iberian Massif) is a Variscan high-P unit mainly constituted by metapelites, … Más