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Microseismic Monitoring and Geomechanical Modelling of CO2 - bris

Microseismic Monitoring and Geomechanical Modelling of CO2 - bris

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4.4. SHEAR WAVE SPLITTING<br />

50<br />

−3<br />

Event Magnitude<br />

−3.2<br />

−3.4<br />

−3.6<br />

−3.8<br />

40<br />

30<br />

20<br />

10<br />

Injection pressure (MPa)<br />

−4<br />

0 20 40 60 80 100<br />

0<br />

120<br />

Time (minutes)<br />

(a)<br />

50<br />

−3<br />

Event Magnitude<br />

−3.2<br />

−3.4<br />

−3.6<br />

−3.8<br />

40<br />

30<br />

20<br />

10<br />

Injection pressure (MPa)<br />

−4<br />

0<br />

0 10 20 30 40 50 60 70<br />

Time (minutes)<br />

(b)<br />

Figure 4.10: Surface injection pressures (dotted line) <strong>and</strong> event magnitudes (crosses) through time<br />

for water (a) <strong>and</strong> CO 2 (b) injection. There appears to be correlation between event magnitudes<br />

<strong>and</strong> injection pressures during both stages. Injection pressures <strong>and</strong> event magnitudes are similar<br />

for both stages, although events are distributed more evenly during water injection.<br />

orientation <strong>of</strong> the ticks represents the fast direction, with horizontal ticks indicating that ψ is parallel<br />

to the S H axis, while the size <strong>of</strong> the ticks indicates the magnitude <strong>of</strong> δV S . Most <strong>of</strong> the arrivals recorded<br />

during Stage 4 have propagated subhorizontally through the reservoir. As such, ψ will represent a<br />

65

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