Results 241 to 250 of about 114,142 (370)

Seismic imaging of a basaltic Lesser Antilles slab from ancient tectonics. [PDF]

Nature
Yang X, Xie Y, Rychert CA, Harmon N, Goes S, Rietbrock A, Lynch L, Members of the VoiLA Working Group.   +7 more
europepmc   +1 more source

Volcanism and Crustal Stress Field. Narrowing of Graben Width near Unzen Volcano: Effect of local thinning of lithosphere.

, 1994
H. Sato, Hiroshi Shimizu, Setsuya Nakada, Shiro Ohmi   +3 more
openalex   +2 more sources

Age of the lithosphere

, 2011
openaire   +2 more sources

Lithospheric Seismic Structure of the Anatolian Plate and Its Implications for Plateau Uplift: Evidence From Joint Inversion of Receiver Functions and Surface Waves

Geochemistry, Geophysics, Geosystems, Volume 26, Issue 8, August 2025.
Abstract High topography (> ${ >} $1 km) on the Anatolian Plate is widely attributed to buoyant mantle support, not just the isostatic response of crustal shortening. However, uncertainties in lithospheric structure hinder attempts to discriminate between competing uplift mechanisms.
Pengzhe Zhou, Ian D. Bastow, Rita Kounoudis, Christopher S. Ogden, Yanghua Wang   +4 more
wiley   +1 more source

Orogenic structure and topography track subduction singularities during slab delemination and detachment. [PDF]

Sci Rep
Handy MR.
europepmc   +1 more source

The Global Sedimentary Basin Stress Project of the International Lithosphere Program

, 1993
J S Bell
openalex   +1 more source

Isostatic response of the Australian lithosphere: Estimation of effective elastic thickness and anisotropy using multitaper spectral analysis [PDF]

, 2000
Frederik J. Simons, M. T. Zuber, Jun Korenaga   +2 more
openalex   +1 more source

Magmatic expressions of continental lithosphere removal

, 2015
Huilin Wang, C. Currie
semanticscholar   +1 more source

Syn‐Rift Magmatism and Oceanic Spreading Initiation Controlled by Rift Obliquity: Insights From 3D Coupled Thermo‐Mechanical and Surface Processes Modeling

Journal of Geophysical Research: Solid Earth, Volume 130, Issue 8, August 2025.
Abstract Continental rifting is often oblique, controlled by various inherited weak crustal and mantle heterogeneities striking at non‐orthogonal angles to the direction of extension. Oblique rifting is known to induce strain partitioning and along‐strike segmentation of the rift structure, but its effects on the magma generation and spreading ...
Éva Oravecz, Attila Balázs, Taras Gerya, Dave A. May, László Fodor   +4 more
wiley   +1 more source

Sulfide-rich continental roots at cratonic margins formed by carbonated melts. [PDF]

Nature
Chen C, Förster MW, Shcheka SS, Ezad IS, Shea JJ, Liu Y, Jacob DE, Foley SF.   +7 more
europepmc   +1 more source