What is he best known for?
The fields of study he is best known for:
- Igneous rock
- Sedimentary rock
- Plate tectonics
Ondrej Lexa mainly investigates Crust, Geochemistry, Massif, Geomorphology and Granulite.
When carried out as part of a general Crust research project, his work on Continental crust is frequently linked to work in Bouguer anomaly, therefore connecting diverse disciplines of study.
His Continental crust research incorporates elements of Passive margin and Oceanic crust.
The study of Geochemistry is intertwined with the study of Nappe in a number of ways.
As a member of one scientific family, Ondrej Lexa mostly works in the field of Geomorphology, focusing on Subduction and, on occasion, Foreland basin.
His biological study spans a wide range of topics, including Eclogite and Protolith.
His most cited work include:
- An Andean type Palaeozoic convergence in the Bohemian Massif (196 citations)
- Chronological constraints on the pre-orogenic history, burial and exhumation of deep-seated rocks along the eastern margin of the Variscan Orogen, Bohemian Massif, Czech Republic (176 citations)
- Vertical extrusion and horizontal channel flow of orogenic lower crust: key exhumation mechanisms in large hot orogens? (148 citations)
What are the main themes of his work throughout his whole career to date?
Ondrej Lexa mainly focuses on Geochemistry, Petrology, Crust, Massif and Paleontology.
His Geochemistry study integrates concerns from other disciplines, such as Subduction, Eclogite and Granulite.
His Granulite research is multidisciplinary, incorporating elements of Anatexis and Protolith.
Ondrej Lexa interconnects Diapir, Mineralogy, Magma and Geomorphology in the investigation of issues within Petrology.
His Continental crust study, which is part of a larger body of work in Crust, is frequently linked to Bouguer anomaly, bridging the gap between disciplines.
His Massif research incorporates themes from Mylonite, Felsic, Lithosphere, Dome and Metamorphic facies.
He most often published in these fields:
- Geochemistry (41.46%)
- Petrology (26.83%)
- Crust (28.46%)
What were the highlights of his more recent work (between 2015-2021)?
- Geochemistry (41.46%)
- Petrology (26.83%)
- Paleontology (17.07%)
In recent papers he was focusing on the following fields of study:
Ondrej Lexa mainly investigates Geochemistry, Petrology, Paleontology, Crust and Continental crust.
His Geochemistry research is multidisciplinary, incorporating perspectives in Granulite, Craton and Continental margin.
His work deals with themes such as Massif, Subduction, Diapir and Lithosphere, which intersect with Petrology.
His Massif study incorporates themes from Lineation and Devonian.
The Crust study which covers Oceanic crust that intersects with Terrane.
The study incorporates disciplines such as Partial melting and Accretionary wedge in addition to Continental crust.
Between 2015 and 2021, his most popular works were:
- Anatexis of accretionary wedge, Pacific‐type magmatism, and formation of vertically stratified continental crust in the Altai Orogenic Belt (36 citations)
- Geochemical and geochronological constraints on distinct Early-Neoproterozoic and Cambrian accretionary events along southern margin of the Baydrag Continent in western Mongolia (35 citations)
- Neoproterozoic‐Early Paleozoic Peri‐Pacific Accretionary Evolution of the Mongolian Collage System: Insights From Geochemical and U‐Pb Zircon Data From the Ordovician Sedimentary Wedge in the Mongolian Altai (29 citations)
In his most recent research, the most cited papers focused on:
- Igneous rock
- Sedimentary rock
- Plate tectonics
His primary areas of investigation include Geochemistry, Crust, Petrology, Continental crust and Granulite.
Ondrej Lexa combines subjects such as Symplectite and Omphacite with his study of Geochemistry.
His studies deal with areas such as Heat transfer and Magma as well as Crust.
His study focuses on the intersection of Continental crust and fields such as Partial melting with connections in the field of Sedimentary rock, Magmatism, Accretionary wedge and Arc system.
His Granulite research is multidisciplinary, relying on both Eclogite, Earth science, Allochthon, Amphibole and Inversion.
His Zircon study combines topics from a wide range of disciplines, such as Fractional crystallization, Subduction, Island arc, Ultramafic rock and Ophiolite.
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