Influence of Inherited Rifted Margin Architecture on Continental Collision Dynamics
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
A small short-necked hupehsuchian from the lower Triassic of Hubei Province, China. [PDF]
Chen XH +4 more
europepmc +1 more source
Hornblendite in the Lower Crust: A Possible Source for Porphyry Cu Deposits
Abstract Lower crustal sulfide‐bearing Cu‐rich cumulates, mainly occurring as hornblendite, have been proposed as a critical source component for the development of giant porphyry Cu deposits (PCDs); however, their mineralogical and geochemical nature remain elusive.
Guangxu Li +5 more
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The Origin of Middle Triassic Thick Anhydrite in the Lower Yangtze Region, South China: Implications for the Evolution of Lithium-Rich Brine. [PDF]
Wu T +7 more
europepmc +1 more source
Crustal and Upper Mantle Structure Beneath the Corinth Rift Using Receiver Function Analysis
Abstract The Gulf of Corinth is one of the fastest‐extending continental rifts in Europe, yet the link between present‐day strain, inherited crustal structure, and lithospheric dynamics remains debated. We investigate crustal thickness and Vp/Vs variations using receiver functions from 31 seismic stations.
Eleni E. Karagianni +2 more
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Study on the genesis mechanism of geothermal resources in the Yunkai area, South China based on geophysical data. [PDF]
Zhou Y +7 more
europepmc +1 more source
Abstract Southern Italy and eastern Sicily have been the site of several destructive historical earthquakes. Here at the junction between the western edge of the Calabrian subduction zone and the Malta Escarpment several strike‐slip faults have been mapped, which may be the surface expression of the lateral slab tear fault and are candidate sources for
M.‐A. Gutscher +4 more
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Habitability at the edge of the redox boundary during the Permian-Triassic mass extinction. [PDF]
Bagherpour B +3 more
europepmc +1 more source
The Upper Permian and the Lower Triassic in Kashmir, India
It has been known since more than seventy years ago that the fossiliferous Permian-Triassic rocks are well developed around the Vihi plain near Srinagar in Kashmir. It is confirmed that the Upper Permian-Lower Triassic boundary is actually conformable and gradational, and that the basal part of the Lower Triassic beds contains survived Permian-type ...
openaire
Abstract Slip rate is a key input for fault‐based seismic hazard assessment, with temporal and spatial variations in slip rate along and between faults influencing earthquake size and recurrence. Temporal variations in slip rate have been attributed to earthquake clustering and anti‐clustering in tectonically active settings.
Billy J. Andrews +6 more
wiley +1 more source

