Fernando Bea

What is he best known for?

The fields of study he is best known for:

• Igneous rock
• Geochemistry
• Volcano

Fernando Bea mainly focuses on Geochemistry, Zircon, Monazite, Partial melting and Mafic. The various areas that Fernando Bea examines in his Geochemistry study include Batholith and Mineralogy. His study in Zircon is interdisciplinary in nature, drawing from both Precambrian and Felsic.

His study looks at the relationship between Monazite and topics such as Plagioclase, which overlap with Biotite, Muscovite and Trace element. His studies deal with areas such as Uraninite and Analytical chemistry as well as Partial melting. The concepts of his Mafic study are interwoven with issues in Massif and Metamorphism.

His most cited work include:

• Residence of REE, Y, Th and U in granites and crustal protoliths : implications for the chemistry of crustal melts (689 citations)
• Mineral/leucosome trace-element partitioning in a peraluminous migmatite (a laser ablation-ICP-MS study) (454 citations)
• Behavior of accessory phases and redistribution of Zr, REE, Y, Th, and U during metamorphism and partial melting of metapelites in the lower crust: an example from the Kinzigite Formation of Ivrea-Verbano, NW Italy (311 citations)

What are the main themes of his work throughout his whole career to date?

His primary scientific interests are in Geochemistry, Zircon, Mafic, Pluton and Felsic. His study in Geochemistry concentrates on Mantle, Anatexis, Partial melting, Massif and Igneous rock. His Zircon research includes elements of Crust, Craton, Metamorphism, Petrology and Archean.

His work carried out in the field of Mafic brings together such families of science as Xenolith, Batholith, Diorite, Gabbro and Underplating. His research in Pluton intersects with topics in Amphibole, Biotite, Plagioclase, Igneous differentiation and Silicic. His Plagioclase research focuses on Monazite and how it connects with Fractional crystallization and Mineralogy.

He most often published in these fields:

• Geochemistry (86.61%)
• Zircon (45.67%)
• Mafic (19.69%)

What were the highlights of his more recent work (between 2016-2021)?

• Geochemistry (86.61%)
• Zircon (45.67%)
• Mafic (19.69%)

In recent papers he was focusing on the following fields of study:

Fernando Bea spends much of his time researching Geochemistry, Zircon, Mafic, Metamorphic rock and Craton. His research investigates the connection with Geochemistry and areas like Pluton which intersect with concerns in Amphibole. His Zircon research includes themes of Gneiss, Mid-Atlantic Ridge, Mantle and Crust.

His work deals with themes such as Xenolith, Biotite, Partial melting and Underplating, which intersect with Mafic. His Metamorphic rock research incorporates elements of Outcrop, Metasomatism, Obduction and Paleozoic. Fernando Bea has researched Craton in several fields, including Massif and Greenschist.

Between 2016 and 2021, his most popular works were:

• Palaeogeography and crustal evolution of the Ossa–Morena Zone, southwest Iberia, and the North Gondwana margin during the Cambro-Ordovician: a review of isotopic evidence (25 citations)
• Lu-Hf ratios of crustal rocks and their bearing on zircon Hf isotope model ages: The effects of accessories (20 citations)
• Geochemical, isotopic, and zircon (U-Pb, O, Hf isotopes) evidence for the magmatic sources of the volcano-plutonic Ollo de Sapo Formation, Central Iberia (13 citations)

In his most recent research, the most cited papers focused on:

• Igneous rock
• Geochemistry
• Volcano

The scientist’s investigation covers issues in Zircon, Geochemistry, Crust, Felsic and Mantle. His biological study spans a wide range of topics, including Subduction, Craton and Mafic. His Subduction research is multidisciplinary, relying on both Continental crust, Metamorphism, Magmatism, Igneous differentiation and Pluton.

Fernando Bea studies Geochemistry, focusing on Greenschist in particular. His studies in Crust integrate themes in fields like Metamorphic rock, Gneiss, Igneous rock and Volcanic rock. His research integrates issues of Allanite, Monazite, Partial melting and Titanite in his study of Felsic.