What is he best known for?
The fields of study he is best known for:
- Sedimentary rock
- Paleontology
- Plate tectonics
The scientist’s investigation covers issues in Geochemistry, Metamorphism, Paleontology, Metamorphic rock and Seismology.
His research in Metamorphism intersects with topics in Coesite, Eclogite and Granulite.
His work carried out in the field of Metamorphic rock brings together such families of science as Devonian and Craton.
His studies in Seismology integrate themes in fields like Massif and Paleozoic.
In his work, Extensional tectonics is strongly intertwined with Cretaceous, which is a subfield of Massif.
His Petrology research incorporates elements of Terrane and Omphacite.
His most cited work include:
- Large areal extent of ultrahigh-pressure metamorphism in the Sulu ultrahigh-pressure terrane of East China: new implications from coesite and omphacite inclusions in zircon of granitic gneiss (226 citations)
- Mesozoic and Cenozoic tectonic history of the central Chinese Tian Shan; reactivated tectonic structures and active deformation (173 citations)
- Neogene uplift of the Tian Shan Mountains observed in the magnetic record of the Jingou River section (northwest China) (106 citations)
What are the main themes of his work throughout his whole career to date?
Qingchen Wang spends much of his time researching Geochemistry, Paleontology, Seismology, Tectonics and Cretaceous.
His work carried out in the field of Geochemistry brings together such families of science as Eclogite and Petrology.
He works mostly in the field of Paleontology, limiting it down to concerns involving Geomorphology and, occasionally, Crust.
Qingchen Wang works mostly in the field of Seismology, limiting it down to topics relating to Early Triassic and, in certain cases, Décollement.
His studies in Cretaceous integrate themes in fields like Paleomagnetism, Anticline and Unconformity.
His work in Metamorphism addresses subjects such as Terrane, which are connected to disciplines such as Zircon.
He most often published in these fields:
- Geochemistry (41.33%)
- Paleontology (38.67%)
- Seismology (26.67%)
What were the highlights of his more recent work (between 2015-2018)?
- Seismology (26.67%)
- Tomography (8.00%)
- Mantle wedge (5.33%)
In recent papers he was focusing on the following fields of study:
His primary areas of investigation include Seismology, Tomography, Mantle wedge, P wave and Petrology.
His research integrates issues of Geochemistry, Transition zone and Massif in his study of Seismology.
His Transition zone course of study focuses on Metamorphism and Subduction.
His research in Petrology intersects with topics in Structural basin, Oil shale, Imbrication and Paleozoic.
He works mostly in the field of Seismic anisotropy, limiting it down to concerns involving Geomorphology and, occasionally, Paleontology.
Qingchen Wang interconnects Shear and Cretaceous in the investigation of issues within Mesozoic.
Between 2015 and 2018, his most popular works were:
- Continuity of the Alpine slab unraveled by high-resolution P wave tomography (51 citations)
- Cenozoic exhumation history of Sulu terrane: Implications from (U–Th)/He thermochrology (28 citations)
- Mantle wedge exhumation beneath the Dora-Maira (U)HP dome unravelled by local earthquake tomography (Western Alps) (23 citations)
In his most recent research, the most cited papers focused on:
- Sedimentary rock
- Plate tectonics
- Paleontology
His primary areas of study are Geochemistry, Mesozoic, Cretaceous, Cenozoic and Seismology.
Qingchen Wang does research in Geochemistry, focusing on Massif specifically.
His Mesozoic research includes elements of Imbrication and Paleozoic.
The Cretaceous study combines topics in areas such as Lineation, Shear, Petrology, Fault and Extensional tectonics.
His Cenozoic research includes themes of Thermochronology, Fission track dating, Zircon and Pacific Plate.
His Seismology research integrates issues from Slab and Metamorphism.
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.
