Matthew J. Comeau

Assistant Professor

Delft University of Technology

Netherlands

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Matthew J. Comeau is an Assistant Professor at Delft University of Technology, Netherlands. His research areas focus on geophysical methods, particularly electrical resistivity and magnetotellurics, to investigate geological structures and processes. Recent articles coalesce around the subsurface characteristics of salt diapirs in Iran, rift propagation in the Tibetan Plateau, and mineral systems imaging in Mongolia.

Matthew J. Comeau

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Articles (16)

The subsurface structure of salt diapirs revealed with electrical resistivity models in the Shurab area, Central Iran

Rift propagation across the Tibetan Plateau as a consequence of fluid flow from south to north

Characterizing the migration of deep materials beneath the Xainza-Dinggye rift and the seismogenic environment in the southern Tibetan Plateau: Insights from a 3-D electrical resistivity model

The emplacement model of the Qitianling pluton in southern Hunan, China: New insights from 3-D magnetotelluric imaging

Crustal conductivity footprint of the Miocene porphyry copper polymetallic deposits in the Gangdese metallogenic belt, Tibetan Plateau

Insights Into the Structure of the Mongol-Okhotsk Suture Zone, Adaatsag Ophiolite, and Tectonic Boundaries of the Central Asian Orogenic Belt (Mongolia) From Electrical Resistivity Imaging and Seismic Velocity Models

Insights Into the Structure of the Mongol‐Okhotsk Suture Zone, Adaatsag Ophiolite, and Tectonic Boundaries of the Central Asian Orogenic Belt (Mongolia) From Electrical Resistivity Imaging and Seismic Velocity Models

Long-Term Stability, Noise, and Temperature Sensitivity of Modular Porous-Pot Electrodes Designed for Geophysical and Geotechnical Applications, and Details of Their Construction

The structure of a continental intraplate volcanic system and controls from shear zones: Insights into the central Hoggar Cenozoic volcanic province, Northwest Africa, from electrical resistivity images

Imaging the Architecture of Mineral Systems and the Pathways of Ore‐forming Fluids across Mongolia with Magnetotellurics

Improved Responses with Multitaper Spectral Analysis for Magnetotelluric Time Series Data Processing: Examples from Field Data

Relationship between the migration of crustal material, normal faulting, and gneiss domes in the vicinity of the Dinggye region, central part of the Tethys- Himalaya terrane: Insights from the 3-D electrical structure

Evidence for partial melting and alkali-rich fluids in the crust from a 3-D electrical resistivity model in the vicinity of the Coqen region, western Lhasa terrane, Tibetan Plateau

Crustal structure of the Lazufre volcanic complex and the Southern Puna from 3-D inversion of magnetotelluric data: Implications for surface uplift and evidence for melt storage and hydrothermal fluids

Crustal structure of the Lazufre volcanic complex and the Southern Puna from 3-D inversion of magnetotelluric data: Implications for surface uplift and evidence for melt storage and hydrothermal fluids

Relationship of the Crustal Structure, Rheology, and Tectonic Dynamics Beneath the Lhasa‐Gangdese Terrane (Southern Tibet) Based on a 3‐D Electrical Model

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