Results 191 to 200 of about 74,650 (313)
Abstract Continental breakup involves multiple extension styles; each linked to unique structural and sedimentary processes. High‐angle, low‐angle, listric and antilistric normal faults develop at different stages and positions during rifting. The Bay of Biscay and its margins, a prototypical example of magma‐poor rifted margins during Jurassic ...
Asier Madarieta‐Txurruka +5 more
wiley +1 more source
Open Access Journals / Institutional Repositories [PDF]
Düpow, Heidi +2 more
core +1 more source
Abstract The continental‐side paleo‐rift structure in the east‐central Korean Peninsula is investigated using joint inversion of receiver functions and surface‐wave dispersions based on dense seismic networks. The joint inversion analysis provides precise constraints on crustal thickness and VP/VS ${V}_{P}/{V}_{S}$ ratios, and high‐resolution 3‐D shear‐
Jeongin Lee +6 more
wiley +1 more source
International Geodynamics Research Center opens in Kyrgyz Republic [PDF]
V. A. Zeigarnik +2 more
openalex +1 more source
A 3D Velocity Model for the European Alps: New Insights Into the Crustal Structure
Abstract We present the first crustal 3D P‐ and S‐wave velocity model covering the entire Greater Alpine region (GAR) based on Local Earthquake tomography. Applying the deep neural network PhaseNet to broad‐band waveforms from 989 stations in the GAR between 2016 and 2022, we determined 173,841 P‐ and 68,967 S‐phase onsets from 2,553 events with ML ${M}
Benedikt Braszus +2 more
wiley +1 more source
Reconstruction of thermally-driven flows using Lagrangian particle data assimilation. [PDF]
Nakao A +4 more
europepmc +1 more source
The geodynamics of Mt. Etna volcano during and after the 1984 eruption
S. La Delfa, G. Patanè, C. Centamore
openalex +2 more sources
Magmatism and Geodynamics: Terrestrial Magmatism Throughout the Earth's History [PDF]
A. F. Koster van Groos
openalex +1 more source
Abstract Hydrogen was first detected in the Bulqizë ophiolite massif (Albania) in 1992, and its origin remains uncertain, with hypotheses ranging from active serpentinization to the release of trapped, fossil H2. To constrain the thickness of the ophiolite layer—a key parameter for evaluating hydrogen generation—we conducted a magnetotelluric survey ...
Yan Yao +8 more
wiley +1 more source

