Results 201 to 210 of about 66,192 (275)
Abstract The Outer California Borderland (OCB) is an active transform plate boundary offshore Southern California, where the relationship between faulting and submarine mass transport deposits (MTDs) remains poorly understood. Onshore paleoseismic data provide high‐resolution earthquake records, whereas marine geophysical data capture longer‐term ...
Andrea Fabbrizzi +3 more
wiley +1 more source
Abstract Constraints on three‐dimensional fault system geometry and kinematics are required to understand both long‐term tectonics and contemporary seismic hazard. In many cases, these parameters must be inferred from a combination of different data or analyses.
A. M. Mere +3 more
wiley +1 more source
Large-scale crustal growth driven by LIP magmatism during the Paleoproterozoic. [PDF]
Simões MS +6 more
europepmc +1 more source
Abstract The Mont Blanc granite, as other deformed granites, has splitting properties attributed to two perpendicular planes: one formed by aligned fractures and the other by aligned micas in foliation planes. It is shown that this microstructure results from ductile deformation with stress‐driven dissolution of quartz and feldspar that passively ...
Jean‐Pierre Gratier +2 more
wiley +1 more source
Archean rifts and triple-junctions revealed by gravity modeling of the southern Superior Craton. [PDF]
Galley C +4 more
europepmc +1 more source
Stress Barriers and Their Impact on Rupture Propagation
Abstract Earthquake ruptures often exhibit complex behaviors, including abrupt arrest followed by delayed re‐nucleation. While on‐fault stress heterogeneity is a recognized contributing factor, as it can arrest or slow down rupture propagation, its interaction with propagating ruptures remains complex and not fully understood. Here, we study frictional
F. Paglialunga +2 more
wiley +1 more source
Geodynamics of a global plate reorganization from topological data analysis. [PDF]
Janin A +3 more
europepmc +1 more source
Abstract The Late Cretaceous Oman ophiolite includes a series of volcanic rocks generated during the transition from spreading ridge to protoarc associated with subduction initiation. We analyzed major and trace elements and Sr, Nd, and Pb isotope compositions of lavas and dikes of the protoarc stage, especially boninites. We also analyzed amphibolites
Tsuyoshi Ishikawa +6 more
wiley +1 more source
Presence of continental slivers in oceanic transform faults determined by rift inheritance. [PDF]
Balázs A, Gerya T, Tari G.
europepmc +1 more source

