In-situ stress analysis of Ahnet Basin, South western Algeria: A 1D geomechanical approach

被引:5
作者
Bouchachi, Youcef [1 ,2 ]
Boudella, Amar [1 ]
Bourouis, Seid [3 ]
Boukhallat, Saad [2 ]
Harbi, Assia [3 ]
机构
[1] Univ Sci & Technol Houari Boumediene, Fac Sci Terre Geog & Amenagement Territoire, Dept Geophys, Lab Geophys, BP 32 El Alia, Bab Ezzouar 16111, Algiers, Algeria
[2] SONATRACH, Algiers 16035, Algeria
[3] Ctr Rech Astron Astrophys & Geophys, BP 63, Bouzareah 16340, Algiers, Algeria
关键词
Present day in -situ stress; 1D geomechanical model; Stress direction; Stress magnitudes; Pore pressure; Fault reactivation; Ahnet basin; Algeria; PRESENT-DAY STATE; PORE PRESSURE; TECTONIC STRESS; TEMPERATURE METAMORPHISM; INDUCED SEISMICITY; FORMAL INVERSION; CENTRAL SAHARA; FIELD; RESERVOIR; CRUSTAL;
D O I
10.1016/j.jafrearsci.2022.104678
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This work aims to determine the present-day in-situ stress and pore pressure in the Ahnet Basin, Algeria, through a 1D geomechanical approach. We investigated the drilling-induced fracture (DIF) from FMI log data to ascertain the direction of maximum horizontal stress (SHmax) from the Ahnet Field. A mean orientation of N140 ( & PLUSMN; 10) has been interpreted, which is NW-SE (N140-N320), with a local variation of ( & PLUSMN; 20) compared to fields such as Illizi, Hassi Messaoud, and North Algeria, which can be explained by depth variation and intrinsic rock properties. A 1.05 psi/ft gradient of overburden stress (Sv) has been obtained from density. Pore pressure has been estimated from the sonic log by a normal compaction trend, indicates a hydrostatic regime from the surface to the top of the Silurian unit with an average pore pressure gradient of 0.43 psi/ft and an overpressure regime against the hot shale unit with a gradient of 0.58 psi/ft caused by the high in situ temperature in the study area and possible activity of the mega-shear zone. The poroelastic approach under transverse isotropic vertical conditions (VTI) has been used to calculate the minimum and maximum horizontal stress magnitudes. The outlines indicate a high-stress gradient close to 0.82 psi/ft, for Shmin calibrated with MDT stress points and 1.10 psi/ft for SHmax. The stress magnitudes results, suggest a present-day normal to strike-slip stress regime in the Ahnet Basin. Fault reactivation potential at two Silurian units has been inferred from the frictional theory analysis. The results indicate that increased pore pressure in hot shale formations due to by fluid injection and hydraulic fracturing causing shear slippage of the pre-existing faults, resulting in induced seismicity. Our study has contributed to the understanding of stress state origin in Ahnet Basin, the relationship between in situ temperature and pore pressure, and the fault stability analysis in such unconventional reservoir development.
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页数:14
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