Characterization of Fault Zones by Analysis of Aftershock Waveform Data波形表,数据分析,余震,表征,故障,地震速度,三维有限差分,S波速度在在一个差错地区和包围岩石的材料之间的大性质对比被重复地震经常生产。差错地区被液体集中,充满泥土的差错凿,增加的孔,和膨胀裂缝通常描绘。因此,差错地区被认为比包围岩石减少了...
Characterization of fault zones. Pure Appl. Geo- phys. 160 (3-4), 677-715.BEN-ZION, Y. and SAMMIS, C. G. (2003), Characterization of fault zones, Pure Appl. Geophys., 160 (3-4), 677-715.BEN-ZION, Y. and SAMMIS, C.G. (2003), Characterization of fault zones, Pure Appl. ...
A challenging task for geothermal exploration is the geothermal characterization of fault zones, which seems to play an important role for the exploration of the geothermal Malm Aquifer in the Munich region. The results of an actualized regional thermo-hydraulic model of the Munich region as well ...
Fault zones are complex, anisotropic, and heterogeneous discontinuities cutting the upper Earth’s crust5. Extensive research has shown that their architecture (e.g. lithology, fault zone geometry, spatial variability), their mechanics (e.g. fault displacement, fluid-rock interactions), and their fl...
Characterization of leaky faults: study of water flow in aquifer-fault-aquifer systems: Chao Shan, I. Javandel & P. A. Witherspoon, Water Resources Research, 31(12), 1995, pp 2897–2904 Characterization of leaky faults in vadose zones of large thickness is very important for engineering probl...
The present work focuses on the mapping and description of onshore brittle fault zones on the SW Barents Sea Margin, within gneisses and granitic intrusions belonging to the West Troms Basement Complex. The description of the brittle structures includes the geometry, kinematics and fault rock charact...
However, these studies have not directly examined the physicochemical characteristics of brittle fault rocks of the youngest active domain in major fault zones. On the other hand, although trench excavation survey (e.g., Benson and Mustoe, 1995; Okada and Tsutsumi, 1997) or mineral vein method ...
Such faults have propagated up from Precambrian basement and thus seem to provide pre-existing zones of weakness available for reactivation. However, the study of seismogenesis in the region has been hampered by the fact that earthquake epicenters frequently do not correlate wi...
of the Salton Trough includes features characteristic of strike-slip faults, such as stepovers, conjugate faults, folds, flower structures, and fault bends, as well as many unique structures that include pooch structures, ramp-flat geometries of strike-slip faults, complex en echelon fault zones ...
Thus, this technique must only be used to improve the sensitivity of a classification scheme when the scheme itself is being used to delineate different zones of rock properties, and not yet, for example, for selection of support and reinforcement. Show moreView chapterExplore book A review of...