Titlebook: Seismicity Associated with Mines, Reservoirs and Fluid Injections; Shahriar Talebi Conference proceedings 1998 Springer Basel AG 1998 Rese

Julienne

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斑駁

極端的正確性

Scaling Laws for the Design of Rock Support,some distance from the source, are developed, based upon theoretical considerations and supported by a world-wide database. These scaling laws reflect the most relevant, critical conditions for engineering design.

exquisite

Seismic and Aseismic Slips Induced by Large-scale Fluid Injections,er than the slip motion associated with microseismic events, as evaluated from events’ magnitude. It is concluded that these observed slip events were aseismic. This implies that induced seismicity is not a good marker for the efficiency of this hydraulic stimulation. It only helps to identify zones of high pore pressure during injection.

系列

Conference proceedings 1998enon include examples of seismicity due to reservoirs, hard-rock mines, coal mines, mine collapses, brine production caverns, fluid injections, and geothermal hot-dry-rock projects. High-frequency acoustic emission studies from laboratory experiments and hard-rock mines have also been reported. Besi

Carminative

Predisposition to Induced Seismicity in Some Czech Coal Mines,s represented by shaft and/or crosscut safety pillars and various types of remnant pillars. All the cases discussed show that many focal zones are generated in overstressed strata as a consequence of interaction of natural conditions and/or old workings with the active coal face.

Acetaldehyde

Spatial Distribution of Mining Tremors and the Relationship to Rockburst Hazard,strated between the location of events, the changes in the state of stress in the massif during the mining operations and the configuration of exploitation. The results have opened interesting perspectives into the analysis of the spatial distribution of mining tremors and their relations to rockburst hazard.

Presbyopia

抱怨

隱語(yǔ)

A Mechanism for High Wall-rock Velocities in Rockbursts,ities associated with the primary seismic events. Whereas varied evidence suggests that slip across a fault at the source of an event generates nearby particle velocities of, at most, several m/s, numerous observations, in nearby damaged tunnels, for instance, imply wall-rock velocities of the order