Results 91 to 100 of about 6,235 (209)
Fault Friction, Plate Rheology, and Mantle Torques From a Global Dynamic Model of Neotectonics
Abstract Improvements in software, parallel computing, global data sets, and laboratory flow‐laws help to develop the global Earth5 thin‐shell finite‐element model of Bird et al. (2008, https://doi.org/10.1029/2007jb005460) into a benchmark study. All experiments confirm that modeled faults (other than megathrusts) have low effective friction of 0.085 ±
Peter Bird +2 more
wiley +1 more source
A Novel Iterative Stable Algorithm for Global Moho Modeling in the Spherical Harmonic Domain
The Mohorovičić discontinuity (Moho) marks the boundary between Earth's crust and the underlying mantle, serving as a critical interface for understanding Earth's structure, composition, and geodynamic processes.
Wenjin Chen, Xiaoyu Tang
doaj +1 more source
Crustal geophysics and seismicity in southern California [PDF]
The geographical distribution of the (1981–2005) seismicity in southern California forms a ±150 km broad zone adjacent to the Pacific–North America plate boundary, ranging from depths of ∼1–~30 km, with the bulk of the focal depths in the range of 2–12 ...
Hauksson, Egill
core +1 more source
Mantle Dynamic Topography of the Fringing Oceanic Basins of Antarctica
Abstract Dynamic mantle processes are known to influence oceanic basins with implications for ocean circulation and climate. This study exploits an interdisciplinary approach to probe present‐day mantle and lithosphere beneath Antarctica's fringing oceanic basins to better understand sub‐crustal processes and implications for the continental realm.
A. C. A. Dunn +4 more
wiley +1 more source
Crustal structure below Popocat\'epetl Volcano (Mexico) from analysis of Rayleigh waves [PDF]
An array of ten broadband stations was installed on the Popocat\'epetl volcano (Mexico) for five months between October 2002 and February 2003. 26 regional and teleseismic earthquakes were selected and filtered in the frequency time domain to extract the
Almendros +27 more
core +7 more sources
Testing Models for Upper Mantle Earthquakes in the Tanganyika‐Rukwa Rift, Africa
Abstract Rifts that initiate in mechanically strong, stable continental lithosphere are characterized by M > 5 earthquakes at depths >35 km near or below the crust mantle interface. Current models for deep rift zone earthquakes invoke elevated pore pressures associated with magmatism, and rapid stressing from magma intrusions.
Eduardo Arzabala +4 more
wiley +1 more source
Estimating the 3D fold structure of the crust-mantel boundary [PDF]
Deep-seated lithospheric folding can be revealed using a method that combines gravity inversion calculations and isostatic analyses.The determination of the crustal structure is essential in geophysics, as it gives insight into the geohistory, tectonic ...
Braitenberg, C. +2 more
core +1 more source
Abstract The opening of the Southwest Sub‐basin (SWSB) of the South China Sea was slow‐spreading and has been propagated toward the southwest. Yet, the structural variability and magmatic accretion process of the SWSB are still enigmatic. Here, utilizing a wide‐angle seismic profile traversing the central segment of the SWSB, we obtain detailed S‐wave ...
Ye Yuan +6 more
wiley +1 more source
Structure and evolution of the Baikal rift: A synthesis [PDF]
Active continental rifts are spectacular manifestations of the deformation of continents but are not very numerous at the surface of the Earth. Among them, the Baikal rift has been extensively studied during the last decades.
Déverchère, Jacques, Petit, Carole
core +4 more sources
Abstract We welcome the critique of Hetényi and Cattin (2026, https://doi.org/10.1029/2025tc009214) on Sternai et al. (2025, https://doi.org/10.1029/2025tc009057), as it brings to light evaluative issues that require clarification and offers an opportunity to articulate more clearly how our work advances understanding of Himalayan‐Tibetan geodynamics ...
P. Sternai +11 more
wiley +1 more source

