What is he best known for?
The fields of study he is best known for:
- Sedimentary rock
- Subduction
- Plate tectonics
J. Casey Moore mainly focuses on Seismology, Subduction, Petrology, Accretionary wedge and Thrust fault.
His biological study spans a wide range of topics, including Ophiolite and Sediment, Geomorphology.
His Petrology research is multidisciplinary, incorporating perspectives in Tectonics, Cataclasite and Underplating.
His Accretionary wedge research includes themes of Fluid dynamics, Anticline, Permeability and Décollement.
The various areas that J. Casey Moore examines in his Décollement study include Neogene, Pelagic sediment and Oceanic crust.
The concepts of his Thrust fault study are interwoven with issues in Ridge and Volcanic arc.
His most cited work include:
- Fluids in accretionary prisms (464 citations)
- Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stress (369 citations)
- Geology of the southern Alaska margin (243 citations)
What are the main themes of his work throughout his whole career to date?
His primary areas of study are Seismology, Accretionary wedge, Subduction, Paleontology and Petrology.
His Seismology study frequently intersects with other fields, such as Borehole.
His Accretionary wedge research incorporates elements of Permeability, Sedimentary rock, Strike-slip tectonics, Seafloor spreading and Underplating.
His research investigates the link between Subduction and topics such as Sediment that cross with problems in Deformation.
His Petrology research is multidisciplinary, incorporating elements of Fluid dynamics, Consolidation, Accretionary complex and Active fault.
His Thrust fault study deals with Canyon intersecting with Anticline.
He most often published in these fields:
- Seismology (51.30%)
- Accretionary wedge (31.30%)
- Subduction (27.83%)
What were the highlights of his more recent work (between 2006-2018)?
- Seismology (51.30%)
- Borehole (14.78%)
- Subduction (27.83%)
In recent papers he was focusing on the following fields of study:
The scientist’s investigation covers issues in Seismology, Borehole, Subduction, Petrology and Thrust fault.
His study in Seismology is interdisciplinary in nature, drawing from both Slip and Seafloor spreading.
He combines subjects such as Graben, Plate tectonics, Horst, Tectonostratigraphy and Décollement with his study of Subduction.
The concepts of his Petrology study are interwoven with issues in Fluid dynamics, Ridge and Diagenesis.
His Thrust fault research integrates issues from Canyon and Overprinting.
His research is interdisciplinary, bridging the disciplines of Deformation and Accretionary wedge.
Between 2006 and 2018, his most popular works were:
- Structure and composition of the plate-boundary slip zone for the 2011 Tohoku-Oki earthquake. (155 citations)
- The thickness of subduction plate boundary faults from the seafloor into the seismogenic zone (89 citations)
- In situ stress state in the Nankai accretionary wedge estimated from borehole wall failures (84 citations)
In his most recent research, the most cited papers focused on:
- Sedimentary rock
- Plate tectonics
- Subduction
J. Casey Moore mostly deals with Seismology, Subduction, Thrust fault, Borehole and Slip.
Plate tectonics, Accretionary wedge, Fault, Earthquake rupture and Décollement are subfields of Seismology in which his conducts study.
His Accretionary wedge study results in a more complete grasp of Tectonics.
His Décollement research is multidisciplinary, incorporating perspectives in Aseismic creep, Petrology, Lithology, Cleavage and Terrane.
His Borehole research is multidisciplinary, incorporating elements of Stress drop, Horizontal stress, Forearc and Stress change.
His Slip research incorporates themes from Strike-slip tectonics and Seafloor spreading.
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