What is he best known for?
The fields of study he is best known for:
- Sedimentary rock
- Igneous rock
- Basalt
His main research concerns Geochemistry, Craton, Archean, Zircon and Crust.
Cristiano Lana has included themes like Basement and Magmatism in his Geochemistry study.
The Craton study combines topics in areas such as Greenstone belt and Continental crust.
His Archean research is multidisciplinary, incorporating perspectives in Gneiss and Terrane.
His research in Zircon intersects with topics in Igneous rock and Back-arc basin.
Mineralogy is closely connected to Geochronology in his research, which is encompassed under the umbrella topic of Monazite.
His most cited work include:
- The ancestry and magmatic evolution of Archaean TTG rocks of the Quadrilátero Ferrífero province, southeast Brazil. (99 citations)
- Stabilization of the southern portion of the São Francisco craton, SE Brazil, through a long-lived period of potassic magmatism (92 citations)
- The Neoarchean transition between medium- and high-K granitoids : Clues from the Southern São Francisco Craton (Brazil) (72 citations)
What are the main themes of his work throughout his whole career to date?
Geochemistry, Zircon, Archean, Craton and Geochronology are his primary areas of study.
By researching both Geochemistry and Rhyacian, he produces research that crosses academic boundaries.
The various areas that Cristiano Lana examines in his Zircon study include Ophiolite, Anatexis, Gondwana and Oceanic crust.
His Archean research incorporates themes from Basement, Gneiss, Continental crust and Paleoarchean.
His Craton study incorporates themes from Siliciclastic, Back-arc basin and Pluton.
His Geochronology research integrates issues from La icp ms, Mineralogy and Magmatism.
He most often published in these fields:
- Geochemistry (70.11%)
- Zircon (35.63%)
- Archean (22.41%)
What were the highlights of his more recent work (between 2018-2021)?
- Geochemistry (70.11%)
- Zircon (35.63%)
- Craton (20.11%)
In recent papers he was focusing on the following fields of study:
Cristiano Lana mainly focuses on Geochemistry, Zircon, Craton, Geochronology and Provenance.
The study incorporates disciplines such as Gondwana and Oceanic crust in addition to Geochemistry.
His Zircon study combines topics from a wide range of disciplines, such as Ophiolite, Mafic, Pluton and Terrane.
Cristiano Lana combines subjects such as Sedimentary depositional environment, Structural basin, Siliciclastic and Recrystallization with his study of Craton.
His biological study spans a wide range of topics, including Crust, Rutile, Brasiliano orogeny and Petrogenesis.
His work on Greenstone belt as part of general Archean research is frequently linked to Rhyacian, bridging the gap between disciplines.
Between 2018 and 2021, his most popular works were:
- The Ribeirao da Folha ophiolite-bearing accretionary wedge (Aracuai orogen, SE Brazil): New data for Cryogenian plagiogranite and metasedimentary rocks (17 citations)
- Metamorphism and exhumation of basement gneiss domes in the Quadrilátero Ferrífero: Two stage dome-and-keel evolution? (16 citations)
- A Neoproterozoic hyper-extended margin associated with Rodinia's demise and Gondwana's build-up : the Araguaia Belt, central Brazil. (15 citations)
In his most recent research, the most cited papers focused on:
- Sedimentary rock
- Basalt
- Igneous rock
Cristiano Lana focuses on Geochemistry, Zircon, Geochronology, Craton and Mafic.
His study in Geochemistry is interdisciplinary in nature, drawing from both Ophiolite and Rodinia.
His Zircon study integrates concerns from other disciplines, such as Subduction, Volcanic arc, Oceanic crust and Terrane.
His Geochronology research is multidisciplinary, incorporating elements of Texture, Igneous rock, Pluton and Petrogenesis.
His Craton study frequently intersects with other fields, such as Siliciclastic.
Within one scientific family, Cristiano Lana focuses on topics pertaining to Provenance under Archean, and may sometimes address concerns connected to Placer mining, Greenstone belt, Banded iron formation and Hydrothermal circulation.
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