What is he best known for?
The fields of study he is best known for:
- Plate tectonics
- Subduction
- Optics
The scientist’s investigation covers issues in Subduction, Seismology, Mantle, Oceanic crust and Lithosphere.
His Subduction study integrates concerns from other disciplines, such as Petrology and Craton.
His Seismology study combines topics in areas such as Deconvolution and Crust.
Many of his studies on Mantle involve topics that are commonly interrelated, such as Seismogram.
The various areas that Michael G. Bostock examines in his Oceanic crust study include Episodic tremor and slip and Plate tectonics.
His Lithosphere study combines topics from a wide range of disciplines, such as Plane wave, Amplitude, Seismic anisotropy, Anisotropy and Classification of discontinuities.
His most cited work include:
- An inverted continental Moho and serpentinization of the forearc mantle (509 citations)
- Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing. (361 citations)
- Mantle stratigraphy and evolution of the Slave province (296 citations)
What are the main themes of his work throughout his whole career to date?
His main research concerns Seismology, Subduction, Mantle, Lithosphere and Geophysics.
In his research, Epicenter and Correlation is intimately related to Low frequency, which falls under the overarching field of Seismology.
His Subduction study deals with Petrology intersecting with Asthenosphere.
His Mantle research is multidisciplinary, relying on both Slab, Tectonics, Thrust fault and Mohorovičić discontinuity.
His Lithosphere research incorporates elements of Seismic anisotropy, Seismic wave, Transition zone and Crust.
His Geophysics research includes themes of Isotropy, Geometry, Scattering and Anisotropy.
He most often published in these fields:
- Seismology (68.33%)
- Subduction (33.33%)
- Mantle (25.00%)
What were the highlights of his more recent work (between 2014-2021)?
- Seismology (68.33%)
- Tectonophysics (10.00%)
- Subduction (33.33%)
In recent papers he was focusing on the following fields of study:
Michael G. Bostock spends much of his time researching Seismology, Tectonophysics, Subduction, Low frequency and Episodic tremor and slip.
Michael G. Bostock conducts interdisciplinary study in the fields of Seismology and Stress drop through his research.
His study in Subduction is interdisciplinary in nature, drawing from both Geophysics, Shear zone, Petrology and Coda.
His work in Petrology addresses subjects such as Oceanic crust, which are connected to disciplines such as Shear.
His research integrates issues of Low-velocity zone and Shear wave splitting in his study of Episodic tremor and slip.
He combines subjects such as Metamorphism, Arc and Forearc with his study of Induced seismicity.
Between 2014 and 2021, his most popular works were:
- Magnitudes and moment‐duration scaling of low‐frequency earthquakes beneath southern Vancouver Island (55 citations)
- Tidal modulation and triggering of low‐frequency earthquakes in northern Cascadia (36 citations)
- Development of a Slow Earthquake Database (28 citations)
In his most recent research, the most cited papers focused on:
- Plate tectonics
- Subduction
- Optics
Michael G. Bostock mainly investigates Seismology, Subduction, Plate tectonics, Petrology and Induced seismicity.
His studies deal with areas such as Low frequency and Free surface as well as Seismology.
His research in Subduction focuses on subjects like Shear zone, which are connected to Outflow, Boundary value problem and Geophysics.
Michael G. Bostock has researched Petrology in several fields, including Arc, Igneous rock and Crust.
The Induced seismicity study combines topics in areas such as Scaling, Transition zone and Geodesy.
His biological study spans a wide range of topics, including Shear wave splitting and High resolution imaging.
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