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Browsing by Author Pereira, M.F.
Showing results 12 to 26 of 26
| Issue Date | Title | Author(s) | | 2021 | Revisiting the Intermediate Sediment Repository Concept Applied to the Provenance of Zircon | Pereira, M.F.; Gama, C. |
| 2021 | Secular variations of magma source compositions in the North Patagonian batholith from the Jurassic to Tertiary: Was mélange melting involved? | Castro, A.; Rodriguez, C.; Fernandez, C.; Aragon, E.; Pereira, M.F.; Molina, J.F. |
| Mar-2018 | Sedimentary provenance of siliciclastic rocks from the Lalla Mouchaa Calcschists Formation (Coastal Block, Western Rehamna): Evidence of denudation of ca. 2 Ga basement in the Moroccan Meseta. | El Houicha, M.; Pereira, M.F.; Jouhari, A.; Gama, C.; Ennih, N.; Fekkak, A.; Ezzouhairi, H.; El Attari, A.; Silva J.B. |
| 2018 | S-type granite generation and emplacement during a regional switch from extensional to contractional deformation (Central Iberian Zone, Iberian autochthonous domain, Variscan Orogeny) | Pereira, M.F.; Díez Fernández, R.; Gama, C.; Hofmann, M.; Gartner, A.; Linnemann, U. |
| 2018 | The Calzadilla Ophiolite (SWIberia) and the Ediacaran fore-arc evolution of the African margin of Gondwana | Arenas, R.; Fernandez-Suarez, J.; Montero, P.; Díez Fernandez, R.; Andonaegui, P.; Sánchez Martínez, S.; Albert, R.; Fuenlabrada, J.M.; Matas, J.; Martín Parra, L.M.; Rubio Pascual, F.J.; Jimenez-Díaz, A.; Pereira, M.F. |
| 2012 | The missing Rheic Ocean magmatic arcs: Provenance analysis of Late Paleozoic | Pereira, M.F.; Chichorro, M.; Johnston, S.T.; Gutierrez-Alonso, G.; Silva, J.B.; Linnemann, U.; Hofmann, M.; Drost, K. |
| 2012 | The provenance of Late Ediacaran and Early Ordovician siliciclastic rocks in the Southwest Central Iberian Zone: Constraints from detrital zircon data on northern Gondwana margin evolution during the late Neoproterozoic | Pereira, M.F.; Linnemann, U.; Hofmann, M.; Chichorro, M.; Solá, A.R; Medina, J.; Silva, J.B. |
| 2022 | The unique Cambro-Ordovician silicic large igneous province of NW Gondwana: Catastrophic melting of a thinned crust | Rodriguez, C.; Castro, A.; Gomez-Frutos, D.; Gutierrez-Alonso, G.; Pereira, M.F.; Fernandez, C. |
| 2018 | Time-space distribution of silicic plutonism in a gneiss dome of the Iberian Variscan Belt: The Évora Massif (Ossa-Morena Zone, Portugal) | Dias da Silva, Í.; Pereira, M.F.; Silva, J.B.; Gama, C. |
| 2021 | Tracking the Late Devonian high-P metamorphic belt in the Variscan Orogen: New constraints on the PT evolution of eclogites from the Cubito-Moura Unit (SW Iberian Massif) | Novo-Fernandez, I.; Arenas, R.; Capitani, Ch.; Pereira, M.F.; Diez Fernandez, R.; Sonia Martinez, S.; Garcia-Casco, A. |
| 2020 | A unique blueschist facies metapelite with Mgrich chloritoid from the Badajoz-Córdoba Unit (SW Iberian Massif): correlation of Late Devonian highpressure belts along the Variscan Orogen | Arenas, R.; Novo-Fernandez, I.; Garcia-Casco, A.; Diez Fernandez, R.; Fuenlabrada, J.M.; Pereira, M.F.; Abati, J.; Sanchez Martinez, S.; Rubio Pascual, F.J. |
| Mar-2018 | U-Pb geochronology of the El Jadida rhyolite and relation to possible Lower Cambrian recycling (Coastal block, Moroccan Meseta). | Pereira, M.F.; Jouhari, A.; El Houicha, M.; Gama, C.; Ezzouhairi, H.; El Attari, A.; Fekkak, A,; Nasser, N.; Silva, J.B. |
| 2021 | Variscan intracrustal recycling by melting of Carboniferous arc-like igneous protoliths (Évora Massif, Iberian Variscan belt) | Rodriguez, C.; Pereira, M.F.; Castro, A.; Gutierrez-Alonso, G.; Fernandez, C. |
| 2021 | Whole‑rock and Sm–Nd isotopic geochemistry of Triassic SW Iberia sandstones: implications for provenance | Gama, C.; Pereira, M.F.; Fuenlabrada, J.M.; Arenas, R. |
| 2019 | Zircon U-Pb geochronology and geochemistry of Cambrian magmatism in the Coastal Block (Oued Rhebar volcanic complex, Moroccan Meseta): Implications for the geodynamic evolutionary model of North-Gondwana | El Attari, A.; Pereira, M.F.; Ezzouhari, H.; El Houicha, M.; Jouhari, A.; Berrada, I.; Fekkak, A.; Ennih, N.; Hoepffner, C.H.; Gama, C.; Silva, J.B. |
Showing results 12 to 26 of 26
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