Three destructive inland earthquakes in the central-western Yamaguchi Prefecture, southwest Japan and accompanied stress changes to their adjacent faultsKanaoriY.TodaS.KoizumiA.ingentaconnectEngineering Geology Amsterdam
The stability of rock mass project is mainly controlled by the rock mass structure,and faults are the large geological discontinuity plane commonly encount... D Huang,H Run-Qiu,YX Zhang - 《Journal of Civil Architectural & Environmental Engineering》 被引量: 18发表: 2009年 389 3D-FEM analysis...
Prediction of fluid flow in hydrocarbon reservoirs is complicated by the presence of faults, which may act as barriers to fluid flow, as conduits for flow, or be partially transmissive. Seismically resolvable faults can be mapped and incorporated explicitly into reservoir evaluation studies, but under...
Krantz RW. Multiple fault sets and three- dimensional strain: theory and application. Journal of Structural Geology. 1988;10: 225-237.KRANTZ R W.Multiple fault sets and three-dimensional strain: Theory and application. Journal of Structural Biology . 1988...
Due to the frequent observation of micro-faults with dominant double cou- ple source mechanism (i.e., shear component), we propose that true 3D stress states can induce rapid weakening on 3D-faults, faster than conventional weakening mechanism(s). This fast-release of energy is associated ...
rock and faults that propagate beneath the surface and control mineralization, as well as the upper and lower limits of surface weather-ing. Th e three-dimensional geometric model using the GoCAD sof t ware served as a powerful tool for the analysis of the geology of the Itataia deposit, ...
The syncline might thus provide a refer- ence section to estimate the original thickness of the Three-dimensional modelling of folds, thrusts, and strike-slip faults in the area of Val de… 617 Fig. 3 Stratigraphic column of Val de Ruz syncline, simplified from Sommaruga (1997). These ...
Fault lubrication and earthquake propagation in thermally unstable rocks Experiments performed on dolomite or Mg-calcite gouges at seismic slip rates (v > 1 m/s)and displacements (d > 1 m) show that the frictional coeffi cient ... N De Paola,T Hirose,T Mitchell,... - 《Geology》 ...
This variability in aspect ratio may either be a consequence of sampling or of underlying geology, but in either case may influence the proportions of relay zones of different types that may be observed on the faults. This topic will be returned to in Section 4.3. Download: Download high-res...
Professor Xiwei XU made a report entitled "Monitoring Experiment of Earthquake Hazard Chain of Active Faults on the South-east Tibetan Plateau", Professor Bin SHI made a report entitled "Theory and techniques of Distributed Optical Fiber Monitoring in Geology and Geotechnical Engineering", Professor Ji...