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Modeling In-situ tectonic stress state and maximum horizontal stress azimuth in the Central Algerian Sahara – A geomechanical study from El Agreb, El Gassi and Hassi Messaoud fields
Gas Science and Engineering ( IF 5.285 ) Pub Date : 2021-02-01 , DOI: 10.1016/j.jngse.2021.103831
Rafik Baouche , Souvik Sen , Rabah Chaouchi , Shib Sankar Ganguli

Central Algerian Sahara hosts many prolific hydrocarbon accumulations in the Paleozoic successions. In this work a contemporary stress field of the Saharan platform has been evaluated using the dataset from recently drilled wells in El Agreb, El Gassi and Hassi Messaoud fields. A pore fluid pressure gradient of 0.56 PSI/feet is interpreted from the in-situ measurements in the Paleozoic reservoir units. Vertical stress (Sv) modeled from the bulk-density data indicates an average of 1.02 PSI/feet gradient. Rock elastic property-based approach is employed to model the magnitudes of minimum (Shmin) and maximum horizontal stress (SHmax) components, which were calibrated with leak off test/minifrac and breakout widths, respectively. Paleozoic stress profiles reveal Shmin/Sv range of 0.74–0.84, while SHmax/Sv varies between 1.1 and 1.33. Subsurface stress distribution indicates that the present-day stress field in the Saharan platform is principally strike-slip faulting (SHmax > Sv > Shmin). A cumulative 1490 m of B-D quality wellbore breakouts, inferred from the acoustic image logs, suggest a NW-SE/WNW-ESE SHmax orientation, which is parallel to the absolute African plate motion and Africa-Eurasia plate convergence direction, implying ridge push force to be the dominant contributor to the tectonic stress field. Mean SHmax orientation shows slightly anticlockwise rotation (126°N to 144°N) from south (El Agreb) to north (Hassi Messaoud field). Inferences are discussed regarding the fault slip potential and hydrocarbon reservoir development.



中文翻译:

模拟中阿尔及利亚撒哈拉沙漠的原地构造应力状态和最大水平应力方位角– El Agreb,El Gassi和Hassi Messaoud油田的地质力学研究

阿尔及利亚中部撒哈拉地区在古生代有许多油气藏。在这项工作中,使用来自最近在El Agreb,El Gassi和Hassi Messaoud井中钻井的数据集评估了Saharan平台的当代应力场。孔隙流体压力梯度为0.56 PSI /英尺,这是根据古生界储层单元的现场测量得出的。根据堆密度数据建模的垂直应力(S v)表示平均值为1.02 PSI /英尺梯度。采用基于岩石弹性特性的方法对最小(S hmin)和最大水平应力(S Hmax)的大小进行建模)组件,分别通过泄漏测试/最小分数和击穿宽度进行校准。古生界应力分布揭示小号HMIN / S v的0.74-0.84范围内,而小号ħ/ S v 1.1和1.33之间变化。地下应力分布表明,撒哈拉平台当前的应力场主要为走滑断层(S Hmax  > S v  > S hmin)。从声波图像测井推断,BD质量井眼累计破裂1490 m,表明NW-SE / WNW-ESE S H m ax方向平行于绝对的非洲板块运动和非洲-欧亚大陆板块的收敛方向,这意味着山脊推力是构造应力场的主要贡献者。平均S Hmax方向显示从南(El Agreb)到北(Hassi Messaoud场)略有逆时针旋转(126°N至144°N)。讨论了有关断层滑动潜力和油气藏开发的推论。

更新日期:2021-02-10
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