2001
DOI: 10.1016/s0040-1951(01)00079-8
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Developing stress-monitoring sites using cross-hole seismology to stress-forecast the times and magnitudes of future earthquakes

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Cited by 28 publications
(37 citation statements)
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“…7, and in changes before earthquakes [25,35,46], the criticality is implied. The only direct observations of extreme compliance are from a prototype stress-monitoring site (SMS) [71] measuring shear-waves in cross-hole seismics between boreholes, adjacent and parallel to the Húsavík-Flatey transform fault of the Mid-Atlantic Ridge in northern Iceland [7]. A calibration test measuring travel times horizontally at 500 m depth between boreholes 315 m-apart happened to coincide with a 4-day swarm of small earthquakes with energy equivalent to a single M ≈ 3.5 earthquake on a parallel transform fault 70 km NNW [7].…”
Section: Critical Systems Of Stress-aligned Fluid-saturated Cracksmentioning
confidence: 99%
“…7, and in changes before earthquakes [25,35,46], the criticality is implied. The only direct observations of extreme compliance are from a prototype stress-monitoring site (SMS) [71] measuring shear-waves in cross-hole seismics between boreholes, adjacent and parallel to the Húsavík-Flatey transform fault of the Mid-Atlantic Ridge in northern Iceland [7]. A calibration test measuring travel times horizontally at 500 m depth between boreholes 315 m-apart happened to coincide with a 4-day swarm of small earthquakes with energy equivalent to a single M ≈ 3.5 earthquake on a parallel transform fault 70 km NNW [7].…”
Section: Critical Systems Of Stress-aligned Fluid-saturated Cracksmentioning
confidence: 99%
“…The expected sensitivity and compliance of the New Geophysics has been directly confirmed by a cross-hole experiment in a prototype borehole Stress-Monitoring Site (SMS) for stress-forecasting earthquakes (Crampin, 2001). The "SMSITES" SMS near the Húsavík-Flatey transform fault of the Mid-Atlantic Ridge in Northern Iceland recorded horizontal seismic travel times at 500 m-depth between boreholes offset 315 m .…”
Section: Direct Evidence Of Rock Sensitivity: the Prototype Stress-momentioning
confidence: 88%
“…The European Commission-funded SMSITES Project is developing a stress-monitoring site (Crampin, 2001) on the onshore extension of the Húsavík-Flatey Fault (HFF), which is a transform fault in the Tjörnes Fracture Zone of the Mid-Atlantic Ridge in Northern Iceland. The aim was to transmit shear waves along specific stress-sensitive directions in order to try to identify the small changes in microcrack geometry, which APE shows are the most immediate effects of accumulating stress, before failure by fracturing occurs.…”
Section: The Stress-monitoring Site Experimentsmentioning
confidence: 99%