Simon Wallis

Professor

University of Tokyo

Japan

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Simon Wallis is a Professor at the University of Tokyo, Japan. His research areas include the evolution of nanocavities in crustal-scale faults, Raman spectroscopy of carbonaceous materials, and the geodynamic processes involved in subduction zones. Recent publications highlight his work on metamorphic rocks and the thermal modeling of tectonic belts, contributing valuable insights into both shear stress and temperature dynamics in geological environments.

Simon Wallis

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Articles (20)

Evolution of Nanocavities to Ductile Fractures in Crustal‐Scale Faults at the Base of the Seismogenic Zone

Paired Metamorphism of SW Japan and Implications for Tectonics of Convergent Margins

Deformation-induced, retrograde transformation of kyanite to andalusite: An example of felsic granulite in the southern Bohemian Massif

Subduction plate interface shear stress associated with rapid subduction at deep slow earthquake depths: example from the Sanbagawa belt, southwestern Japan

An automatic peak deconvolution code for Raman spectra of carbonaceous material and a revised geothermometer for intermediate- to moderately high-grade metamorphism

Implications of Surface Heat Flux for Shear Stress and Temperature on the Plate Interface Beneath Northern Honshu

Geochronology of the Sanbagawa Belt: Younger and Faster than Before

Relation between rheological properties and the stress state in subducting slabs

Thermal Modeling of the Sanbagawa and Ryoke Belts

Identifying plutons associated with long-lived volcanism by thermal modeling of contact metamorphic aureoles

Dehydration of brucite + antigorite under mantle wedge conditions: insights from the direct comparison of microstructures before and after experiments

Recognition of Detrital Carbonaceous Material in the Ryoke Metamorphic Belt by Using Raman Thermometry: Implications for Thermal Structure and Detrital Origin

Recognition of broad thermal anomaly around the median tectonic line in central Kii peninsula, southwest Japan: Possible heat sources

Thermal structure in subducted units from continental Moho depths in a palaeo subduction zone, the Asemigawa region of the Sanbagawa metamorphic belt, SW Japan

The basement geology of Japan from A to Z

Crystallographic preferred orientation of talc determined by an improved EBSD procedure for sheet silicates: Implications for anisotropy at the slab-mantle interface due to Si-metasomatism

Comment on 'Metamorphic olivine after dehydration embrittlement in Serpentinite: Case study from the Shiraga Serpentinite mass in the Sanbagawa high P/T metamorphic belt, central Shikoku, Japan' by Fukumura, Okamoto and Terabayashi, https://doi.org/10.1111/iar.12293

Attenuated total reflection infrared (ATR-IR) spectroscopy of antigorite, chrysotile, and lizardite

High- and low-stress subduction zones recognized in the rock record

Petrogenesis of the Higashi-Akaishi Ultramafic Body: Implications for Lower Crustal Foundering and Mantle Wedge Processes

Collaborators (10)

Ryosuke Oyanagi

Akira Miyake

Atsushi Okamoto

YUSUKE SETO

Takayoshi Nagaya

Hiroshi Mori

Mutsuki Aoya

Masaki ENAMI

Jun Muto

Takamoto Okudaira

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