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3 o W<br />

64 o N<br />

Stress trajectories<br />

a. b.<br />

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1<br />

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c.<br />

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Modeled S hmin /S v<br />

0.75<br />

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0.85<br />

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Observed S hmin /S v<br />

0.75<br />

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0.85<br />

0.8<br />

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Figure 9.3. Comparison between observed directions of maximum horizontal stress in the northern North Sea<br />

and calculated stress directions incorporating the effects of lithospheric flexure due to removal of the<br />

Fennoscandian ice sheet (Grollimund and Zoback 2003). (a) The model accurately reproduces stress<br />

orientations in the northern North Sea. (b) The calculated stress magnitudes are shown as the ratio of the<br />

minimum horizontal stress to the overburden. (c) The magnitude of the minimum horizontal stress as<br />

determined from leak-off tests in wells is quite similar to that predicted by the model. AAPG C○ 2003 reprinted<br />

by permission of the AAPG whose permission is required for futher use.<br />

a. b.<br />

c.<br />

31 31.5 32<br />

32 34 36 38 40 44 46 48 50 52<br />

Required P m Required P m<br />

Required P m<br />

Figure 10.4. The effects of wellbore trajectory and stress state on wellbore stability. The parameters used in<br />

this figure are the same as those used for the calculations shown in Figure 8.2. The figure shows the mud<br />

pressure (in ppg) required to drill a stable well (maximum breakout width 30 ◦ for a relatively strong rock<br />

(UCS ∼50 MPa) as a function of well orientation at a depth of 3 km for hydrostatic pore pressure: (a) normal<br />

faulting, (b) strike-slip faulting and (c) reverse faulting.

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