What is he best known for?
The fields of study he is best known for:
- Sedimentary rock
- Composite material
- Paleontology
Pressure solution, Mineralogy, Creep, Quartz and Compaction are his primary areas of study.
Geotechnical engineering covers Jean-Pierre Gratier research in Pressure solution.
His studies in Mineralogy integrate themes in fields like Surface roughness, Porosity and Surface tension.
Jean-Pierre Gratier has researched Creep in several fields, including Deformation mechanism and Brittleness.
His research integrates issues of Strain rate, Diagenesis and Deformation in his study of Quartz.
His studies examine the connections between Compaction and genetics, as well as such issues in Grain size, with regards to Sedimentary rock.
His most cited work include:
- Kinetics of crack-sealing, intergranular pressure solution, and compaction around active faults (156 citations)
- Pressure solution in sandstones: influence of clays and dependence on temperature and stress (145 citations)
- The Role of Pressure Solution Creep in the Ductility of the Earth’s Upper Crust (128 citations)
What are the main themes of his work throughout his whole career to date?
His scientific interests lie mostly in Pressure solution, Mineralogy, Fault, Creep and Seismology.
Jean-Pierre Gratier has included themes like Active fault and Aseismic creep in his Pressure solution study.
When carried out as part of a general Mineralogy research project, his work on Diagenesis is frequently linked to work in Layering, therefore connecting diverse disciplines of study.
His biological study spans a wide range of topics, including Natural, Quaternary and Petrology.
His studies deal with areas such as Stress, Deformation, Calcite, Displacement and Cleavage as well as Creep.
The Seismology study combines topics in areas such as Deformation mechanism and Slip.
He most often published in these fields:
- Pressure solution (46.32%)
- Mineralogy (26.32%)
- Fault (32.63%)
What were the highlights of his more recent work (between 2014-2019)?
- Fault (32.63%)
- Geotechnical engineering (27.37%)
- Split-Hopkinson pressure bar (12.63%)
In recent papers he was focusing on the following fields of study:
The scientist’s investigation covers issues in Fault, Geotechnical engineering, Split-Hopkinson pressure bar, Pressure solution and Paleontology.
His Fault research integrates issues from Creep and Petrology.
In Geotechnical engineering, he works on issues like Strain rate, which are connected to Compaction.
Jean-Pierre Gratier focuses mostly in the field of Compaction, narrowing it down to matters related to Nucleation and, in some cases, Permeability.
His Pressure solution study necessitates a more in-depth grasp of Mineralogy.
His work in the fields of Paleontology, such as Pleistocene, Quaternary, Crust and Sedimentary rock, intersects with other areas such as Thermodynamic state.
Between 2014 and 2019, his most popular works were:
- Dynamic fracturing by successive coseismic loadings leads to pulverization in active fault zones (57 citations)
- Dynamic fracturing by successive coseismic loadings leads to pulverization in active fault zones (57 citations)
- Evolution of fault permeability during episodic fluid circulation: Evidence for the effects of fluid–rock interactions from travertine studies (Utah–USA) (37 citations)
In his most recent research, the most cited papers focused on:
- Sedimentary rock
- Composite material
- Paleontology
His primary areas of study are Split-Hopkinson pressure bar, Geotechnical engineering, Fault, Active fault and Chronology.
The study incorporates disciplines such as Petrophysics, Earthquake rupture, Perpendicular and Elastic modulus in addition to Split-Hopkinson pressure bar.
His Fault study combines topics in areas such as Petrology, Pressure solution and Cleavage.
His work carried out in the field of Active fault brings together such families of science as Creep, Aseismic creep and Fault gouge.
His Chronology research incorporates themes from Aragonite, Outcrop, Structural geology and Petrography.
His work deals with themes such as Permeability and Crust, which intersect with Petrography.
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