What is he best known for?
The fields of study he is best known for:
- Plate tectonics
- Sedimentary rock
- Subduction
Gérard M. Stampfli spends much of his time researching Paleontology, Terrane, Plate tectonics, Gondwana and Paleozoic.
Ordovician, Passive margin and Subduction are the primary areas of interest in his Paleontology study.
His work carried out in the field of Terrane brings together such families of science as Devonian and Back-arc basin.
His Back-arc basin research is multidisciplinary, relying on both Continental drift, Convergent boundary, Flysch and Greenschist, Metamorphism.
His study in Plate tectonics is interdisciplinary in nature, drawing from both Slab, Foreland basin, Slab window and Accretionary wedge.
His work in Paleozoic addresses subjects such as Permian, which are connected to disciplines such as Thermal subsidence, Volcanic passive margin and Rift.
His most cited work include:
- A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons (1747 citations)
- The Altaids of Central Asia: A tectonic and evolutionary innovative review (464 citations)
- Tethyan margins in space and time (391 citations)
What are the main themes of his work throughout his whole career to date?
Paleontology, Plate tectonics, Terrane, Gondwana and Paleozoic are his primary areas of study.
His study in Subduction, Passive margin, Cretaceous, Permian and Rift are all subfields of Paleontology.
His research integrates issues of Tectonic phase, Cenozoic, Geomorphology and Accretionary wedge in his study of Plate tectonics.
His research investigates the link between Terrane and topics such as Flysch that cross with problems in Siliciclastic.
The study incorporates disciplines such as Massif, Basement and Ordovician in addition to Gondwana.
His work in Paleozoic addresses issues such as Devonian, which are connected to fields such as Metamorphism.
He most often published in these fields:
- Paleontology (71.05%)
- Plate tectonics (32.89%)
- Terrane (26.32%)
What were the highlights of his more recent work (between 2009-2021)?
- Paleontology (71.05%)
- Terrane (26.32%)
- Plate tectonics (32.89%)
In recent papers he was focusing on the following fields of study:
His primary areas of study are Paleontology, Terrane, Plate tectonics, Gondwana and Paleozoic.
His Paleontology research focuses on Cretaceous, Subduction, Tectonics, Basement and Devonian.
His Subduction research incorporates elements of Lithosphere and Continental margin.
His work deals with themes such as Nappe, Flysch, Permian, Accretion and Ordovician, which intersect with Terrane.
As a part of the same scientific family, Gérard M. Stampfli mostly works in the field of Plate tectonics, focusing on Facies and, on occasion, Volcano, Accretionary complex, Seamount and Diachronous.
His studies in Gondwana integrate themes in fields like Promontory, Seafloor spreading, Passive margin and Cenozoic.
Between 2009 and 2021, his most popular works were:
- The Altaids of Central Asia: A tectonic and evolutionary innovative review (464 citations)
- The formation of Pangea (358 citations)
- Pre-Mesozoic Alpine basements - Their place in the European Paleozoic framework (145 citations)
In his most recent research, the most cited papers focused on:
- Plate tectonics
- Sedimentary rock
- Subduction
His primary scientific interests are in Paleontology, Terrane, Gondwana, Plate tectonics and Subduction.
His Paleozoic, Tectonics and Hypsometry study in the realm of Paleontology interacts with subjects such as Flood myth.
His Terrane study integrates concerns from other disciplines, such as Accretion, Ordovician, Basement and Continental margin.
His studies examine the connections between Gondwana and genetics, as well as such issues in Passive margin, with regards to Slab window, Oceanic crust, Ridge and Geodynamics.
His Plate tectonics research includes themes of Facies, Accretionary complex, Volcano and Seamount.
The study incorporates disciplines such as Orogeny, Cretaceous, Fold, Mesozoic and Lithosphere in addition to Subduction.
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