Eastern Himalayan syntaxis formation controlled by slab flattening and crustal shear localization. [PDF]
Nat Geoscivan Agtmaal L +4 more
europepmc +1 more source
Reply to Discussion by R. A. Henderson of 'Kinematics of the Clarke River Shear Zone (northeastern Australia) and implications for the tectonic evolution of the Tasmanides'. [PDF]
Aust J Earth SciRodrigues RT, Rosenbaum G.
europepmc +1 more source
Utilizing 45 years of instrumental seismicity to investigate blind seismogenic faults in Southeastern Piedmont. [PDF]
Sci RepGuiñez-Rivas F +4 more
europepmc +1 more source
Numerical simulation of the seismic response of corroded pipelines crossing faults. [PDF]
Sci RepLi Y, Zhang A.
europepmc +1 more source
Construction of fault geometry by finite-fault inversion of teleseismic data
Construction of fault geometry by finite-fault inversion of teleseismic dataopenaire +1 more source
Fault-surface geometry controlled by faulting mechanisms: Experimental observations in limestone faults [PDF]
Geology, 2017 Surface geometry is an essential component in faulting and earthquake dynamics, yet its evolution and interrelationship with friction are poorly understood. The geometric characteristics of smooth fault surfaces are herein investigated by combining direct shear experiment results with statistical analysis of the surface topography.
Sagy, Amir +2 more
openaire +1 more source
Related searches:
Hierarchical geometry of faulting
Journal of Geophysical Research: Solid Earth, 1996Several joint and fault patterns were mapped at different scales (from 1 cm to 100 km) on the sedimentary cover of Saudi Arabia. They were analyzed using a new multifractal algorithm improved to correct for irregular geometry of mapped domains and finite size effects.
G. Ouillon, C. Castaing, D. Sornette
openaire +1 more source
This meeting took place at Burlington House on 14 and 15 June 1989. Until recently a specialist structural geology meeting on a theme such as this would have been solely the preserve of the Tectonic Studies Group.
ALAN ROBERTS +2 more
openaire +1 more source
Sediment geometries and domino faulting
Geological Society, London, Special Publications, 1993Abstract A general forward modelling scheme is used to produce a model of sediment geometry in half-grabens formed during extension of domino fault blocks. The model includes the effects of erosion, sediment transport, sedimentation and isostasy and simulates both syn- and post-rift sedimentary sequences.
David Waltham +2 more
openaire +1 more source
The impact of fault surface 3D geometry on risking fault reactivation
2023The reactivation of faults can occur when the effective stresses acting on them are perturbed. In some cases man-made changes in effective stress can result in fault reactivation that can have enormous impacts including loss of integrity of underground storage facilities. Current practical methods for making this assessment are generally based on shear
Janis Aleksans +2 more
openaire +1 more source