Results 41 to 50 of about 236 (132)

Arc Heat Flow and Magmatic Heat Budgets

Reviews of Geophysics, Volume 64, Issue 2, June 2026.
Abstract We evaluate hydrothermal heat loss from 11 volcanic‐arc segments (∼6,000 km of arc length, ∼10% of the global total), motivated by the observation that much magmatic heat ultimately crosses the land surface as heated aqueous fluid. Heat loss takes place by volcanic eruption, geothermal heat conduction to the surface, fumarolic (vapor ...
S. E. Ingebritsen, Kazuki Sawayama, Yuri Taran, Giovanni Chiodini, Tsuneomi Kagiyama, Hiroshi Shinohara, Julie V. Rowland, Benjamin A. Black   +7 more
wiley   +1 more source

Geophysical-petrological model for bidirectional mantle delamination of the Adria microplate beneath the Apennines and Dinarides orogenic systems

, 2023
In this study we present a geophysical-geochemical integrated model of the thermochemical structure of the lithosphere and uppermost mantle of the Adria and Tisza microplates along two transects running from the Northern Apennines to the Pannonian Basin, and from the Southern Apennines to the Balkanides, respectively.
Ivone Jimenez-Munt, Wentao Zhang, Montserrat Torné, Jaume Vergés, Estefanía Bravo-Gutierrez, Ana M Negredo, Eugenio Carminati, Daniel Garcia-Castellanos   +7 more
openaire   +2 more sources

Influence of Inherited Rifted Margin Architecture on Continental Collision Dynamics

Geochemistry, Geophysics, Geosystems, Volume 27, Issue 5, May 2026.
Abstract Continental collision is a key process in lithospheric evolution, driving mountain building, crustal thickening, and supercontinent assembly. Within the Wilson cycle, collision marks the final stage following rifting, ocean spreading, and subduction.
J. B. Ruh, P. Granado
wiley   +1 more source

Tectonic Interplay in the Gulf of Cagliari (Italy): Extension, Compression and Strike‐Slip Movements

Basin Research, Volume 38, Issue 3, May–June 2026.
Since the Oligocene, extensional tectonics of the Sardinia Rift and Campidano Graben interacted with the collision between Sardinia and northern Africa, generating reverse faults. At the Plio‐Quaternary boundary, compressional tectonics resumed, shaping the southern margin of the gulf through transpressional tectonics of the exposed Ichnusa High ...
Anna Del Ben, Silvana Fais, Riccardo Geletti, Maria Cristina Caradonna, Veronica Frisicchio, Giuseppe Brancatelli   +5 more
wiley   +1 more source

3‐D Modeling of Differential Exhumation of Ultrahigh‐Pressure Metamorphic Rocks Driven by Increasing Plate Divergence

Geochemistry, Geophysics, Geosystems, Volume 27, Issue 3, March 2026.
Abstract Petrological and seismic constraints suggest differential sampling depth for ultrahigh pressure (UHP) metamorphic rocks exposed in different segments of the fossil subduction zone of the Western Alps. However, the mechanisms for the observed differential exhumation remain to be understood. Here, we account for the continental margin subduction
Xinxin Wang, Liang Zhao, Marco G. Malusà, Weiqiang Ji, Jie Yuan   +4 more
wiley   +1 more source

The bases for understanding of the NW Dinarides and Istria Peninsula tectonics

Geologija, 2010
Thrust structure of the northeastern part of the External Dinarides is depended upon paleogeography of the Adriatic–Dinaric Mesozoic Carbonate Platform, which was in the southeast (in the recent position) composed of Dinaric and Adriatic segment with ...
Ladislav Placer, Marko Vrabec, Bogomir Celarc   +2 more
doaj  

Earthquake Source Depth Determination Using Single Station Waveforms and Deep Learning

Journal of Geophysical Research: Machine Learning and Computation, Volume 3, Issue 1, February 2026.
Abstract In areas with limited station coverage, earthquake depth constraints are much less accurate than their latitude and longitude. Traditional travel‐time‐based location methods struggle to constrain depths due to imperfect station distribution and the strong trade‐off between source depth and origin time.
Wenda Li, Miao Zhang
wiley   +1 more source

Principles of the tectonic subdivision of Slovenia

Geologija, 2008
New tectonic subdivision of the junction region between Alps and Dinarides which incorporates Eastern Alps, Southern Alps, Dinarides, Pannonian basin and Adriatic-Apulia foreland is described in this article.
Ladislav Placer
doaj  

How Fluid Pressures and Viscous Rheologies Affect Slip Patterns on Low‐Angle Normal Faults: The Example of the Altotiberina Fault, Northern Apennines, Italy

Journal of Geophysical Research: Solid Earth, Volume 130, Issue 10, October 2025.
Abstract Low‐angle normal faults are a mechanical anomaly, hosting normal‐sense slip despite having a dip shallower than 30°, in contravention of Andersonian prediction. Slip on such faults has been attributed to overpressurized fluids or low‐friction minerals. An example of such a fault is the Altotiberina Fault (ATF) in central Italy. The ATF hanging
John N. Hooker, Hannah Riegel, Francesco Mirabella, Gabriele Casale   +3 more
wiley   +1 more source

Geological and Tectonic Characteristics and Seismicity of the Kurbnesh-Kukës-Prizren Fault

Albanian Journal of Natural and Technical Sciences
Albania and Kosovo are situated within the seismically active Alpine-Mediterranean belt, where significant crustal deformation results from the ongoing convergence between the Adria microplate and the Eurasian plate.
Naser Peci, Rrapo Ormeni, Behxhet Shala, Petraq Naqo, Dionald Muçaj   +4 more
doaj   +1 more source