-
oa Generation of in-Situ Stress Map in Gulf of Suez (GOS) and Its Impact from Drilling High Angle Wells, Egypt
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, GEO 2010, Mar 2010, cp-248-00201
Abstract
The effect of magnitude and pattern of earth’s in situ stress is generally manifested on the shape of the<br>borehole in a drilled well. It is well known that the stress around the wellbore causes deformation<br>depending on many factors ranging from rock strength to the deviation of the wellpath.<br>In this paper, a stress map is generated from borehole breakout along with other wireline logs from a<br>reasonably large database. Both vertical and deviated wells covering major part of GoS are considered<br>for this study. The fact that stress related breakout originates from the maximum tangential stress is<br>the main criterion here. The tangential stress is combination of forces like earth in situ stresses, drilled<br>mud weight and pore-pressure of the formation. Complimentary to the magnitude, breakout<br>orientation indicates the direction of minimum in situ stress in case of vertical wells. Stress evaluation<br>in deviated wells requires multiple well input in a limited area to generate a stress tensor diagram that<br>determines stress orientations with confidence. In a deviated well the breakout direction is controlled<br>by in situ stress with respect to the trajectory of the well. The study reveals that the min horizontal<br>stress (Sh) in GoS is aligned along two major trends. First, the main NNE - SSW trend, with an<br>average orientation of 10degN exists in most of the part. The second trend is aligned NE - SW and has<br>been observed locally at the central eastern and south-western part of GoS, with an average<br>orientation of 50degN. Most studies of the structural and tectonic history of the GoS have concluded<br>two age significant orientations for this extensional rift. The early to middle Miocene rifting, yielded Sh<br>direction of 55-60degN (rift-climax phase). The younger stress fields of the Late Miocene and Pliocene<br>times rotated progressively counterclockwise and yielded a 15-25degN direction that persisted into<br>early-late Pleistocene time. The main trend therefore is mainly controlled by this younger stress field of<br>the GoS rifting.