What is he best known for?
The fields of study he is best known for:
- Sedimentary rock
- Paleontology
- Plate tectonics
Ulf Linnemann mostly deals with Paleontology, Gondwana, Paleozoic, Ordovician and Zircon.
His Passive margin study in the realm of Paleontology connects with subjects such as Collision.
As a part of the same scientific family, Ulf Linnemann mostly works in the field of Gondwana, focusing on Supercontinent and, on occasion, Pangaea.
His Paleozoic research includes themes of Orogeny and Suture.
His study looks at the relationship between Ordovician and topics such as Provenance, which overlap with Basement.
His biological study spans a wide range of topics, including Massif, Structural basin and Archean.
His most cited work include:
- Evolution of the Rheic Ocean (412 citations)
- The Cadomian Orogeny and the opening of the Rheic Ocean: The diacrony of geotectonic processes constrained by LA-ICP-MS U–Pb zircon dating (Ossa-Morena and Saxo-Thuringian Zones, Iberian and Bohemian Massifs) (294 citations)
- West African provenance for Saxo-Thuringia (Bohemian Massif): Did Armorica ever leave pre-Pangean Gondwana? – U/Pb-SHRIMP zircon evidence and the Nd-isotopic record (279 citations)
What are the main themes of his work throughout his whole career to date?
The scientist’s investigation covers issues in Zircon, Paleontology, Geochemistry, Provenance and Gondwana.
His Zircon research includes elements of Craton, Geochronology, Massif, Devonian and Archean.
His work in Paleozoic, Ordovician, Passive margin, Terrane and Supercontinent are all subfields of Paleontology research.
His work investigates the relationship between Geochemistry and topics such as Basement that intersect with problems in Sedimentary depositional environment.
His Provenance study integrates concerns from other disciplines, such as Sedimentary rock, Sedimentology, Siliciclastic and Cretaceous.
His Gondwana research is multidisciplinary, incorporating perspectives in Orogeny, Rift, Carboniferous and Suture.
He most often published in these fields:
- Zircon (52.78%)
- Paleontology (47.92%)
- Geochemistry (45.83%)
What were the highlights of his more recent work (between 2019-2021)?
- Geochemistry (45.83%)
- Zircon (52.78%)
- Provenance (36.81%)
In recent papers he was focusing on the following fields of study:
His main research concerns Geochemistry, Zircon, Provenance, Geochronology and Paleozoic.
The concepts of his Geochemistry study are interwoven with issues in Gondwana, Permian, Craton and Carboniferous.
The study incorporates disciplines such as Transtension, Orogeny, Allochthon and Terrane in addition to Zircon.
His Provenance course of study focuses on Cretaceous and Structural basin, Heavy mineral, Supercontinent and Marine transgression.
His Paleozoic study contributes to a more complete understanding of Paleontology.
His research ties German and Paleontology together.
Between 2019 and 2021, his most popular works were:
- Late Paleozoic–early Mesozoic continental biostratigraphy — Links to the Standard Global Chronostratigraphic Scale (32 citations)
- Polyphase magmatic pulses along the Northern Gondwana margin: U-Pb zircon geochronology from gneiss domes of the Pyrenees (5 citations)
- Chronostratigraphic framework and provenance of the Ossa-Morena Zone Carboniferous basins (SW Iberia) (4 citations)
In his most recent research, the most cited papers focused on:
- Sedimentary rock
- Paleontology
- Plate tectonics
His primary areas of investigation include Geochemistry, Zircon, Paleozoic, Provenance and Foreland basin.
His Zircon research is multidisciplinary, incorporating elements of Permian, Craton and Orogeny.
Ulf Linnemann focuses mostly in the field of Paleozoic, narrowing it down to topics relating to Carboniferous and, in certain cases, Unconformity, Siliciclastic, Conglomerate and Dike.
His work on Gondwana expands to the thematically related Provenance.
His research in Gondwana intersects with topics in Sedimentary rock, Sedimentology and Cretaceous.
His study in Foreland basin is interdisciplinary in nature, drawing from both Massif, Ordovician and Allochthon.
This overview was generated by a machine learning system which analysed the scientist’s
body of work. If you have any feedback, you can
contact us
here.
