scispace - formally typeset
M

Mathias Obrebski

Researcher at Lamont–Doherty Earth Observatory

Publications -  21
Citations -  928

Mathias Obrebski is an academic researcher from Lamont–Doherty Earth Observatory. The author has contributed to research in topics: Crust & Subduction. The author has an hindex of 14, co-authored 20 publications receiving 846 citations. Previous affiliations of Mathias Obrebski include Institut de Physique du Globe de Paris & Ensenada Center for Scientific Research and Higher Education.

Papers
More filters
Journal ArticleDOI

Lithosphere-asthenosphere interaction beneath the western United States from the joint inversion of body-wave traveltimes and surface-wave phase velocities

TL;DR: In this article, a multiphase DNA10-S model was used to image and study the link between the geology of the western United States, the shallow structure of the Earth and the convective processes in mantle.
Journal ArticleDOI

Slab-plume interaction beneath the Pacific Northwest

TL;DR: In this article, the authors show new high-resolution tomographic images obtained using shear and compressional data from the ongoing USArray deployment that demonstrate first that there is a continuous, whole-mantle plume beneath the Yellowstone Snake River Plain (YSRP) and second, that the subducting Juan de Fuca (JdF) slab is fragmented and even absent beneath Oregon.
Journal ArticleDOI

Seismic anisotropy beneath Cascadia and the Mendocino triple junction: Interaction of the subducting slab with mantle flow

TL;DR: In this article, the Mendocino and FACES seismic networks were used to characterize the mantle flow associated with the Cascadia subduction zone and the triple junction of the Gorda slab.
Journal ArticleDOI

From seismic noise to ocean wave parameters: General methods and validation

TL;DR: In this paper, the authors used a model of noise generation and propagation to separate seismic stations into those that are mostly sensitive to local sea states, and those that integrate sources from a large oceanic area.