Estimation of horizontal stresses from wellbore failures in strike-slip tectonic regime: A case study from the Ordovician reservoir of the Tinzaouatine field, Illizi Basin, Algeria

dc.contributor.authorBaouche, Rafik
dc.contributor.authorSen, Souvik
dc.contributor.authorHadj Arab, Feriel
dc.contributor.authorAhmed, Radwan
dc.date.accessioned2023-09-21T12:43:44Z
dc.date.available2023-09-21T12:43:44Z
dc.date.issued2022
dc.description.abstractWe present a geomechanical analysis of the Ordovician reservoir from the Tinzaouatine field situated in the prolific Illizi Basin, eastern Algeria. The sandstone reservoir has a hydrostatic pore pressure gra- dient (9.95 MPa/km). We analyzed a cumulative of 300 m of acoustic image log data and identified the coexistence of B-quality extensive drilling-induced tensile failures (DITFs) and compressive failures, i.e., breakouts (BOs), indicating a mean maximum horizontal stress (SHMax) orientation of N140°E. We used a combined BO and DITF-based solution to estimate horizontal stress magnitudes when the two failure types coexist. Based on the C-quality minifrac measurements, we interpreted the minimum horizontal stress (Shmin) gradient as 17.4–17.47 MPa/km, whereas the new approach indicates an Shmin range of 17.31–18.67 MPa/km. Using the BO width and DITF-based approaches, we inferred an SHMax gradient range of 28.37–38.59 MPa/km within the studied reservoir. Based on the relative stress magnitudes, we infer a strike-slip tectonic stress regime in the studied field.en_US
dc.identifier.issn2324-8866
dc.identifier.uriDOI:10.1190/int-2021-0254.1
dc.identifier.urihttps://dspace.univ-boumerdes.dz/handle/123456789/12063
dc.language.isoenen_US
dc.publisherSociety of Exploration Geophysicistsen_US
dc.relation.ispartofseriesInterpretation/Vol. 10, N°3 (August 2022);pp. 37–44
dc.subjectHorizontal stressesen_US
dc.subjectOrdovician reservoiren_US
dc.subjectTinzaouatine fielden_US
dc.subjectIllizi Basin, Algeriaen_US
dc.titleEstimation of horizontal stresses from wellbore failures in strike-slip tectonic regime: A case study from the Ordovician reservoir of the Tinzaouatine field, Illizi Basin, Algeriaen_US
dc.typeArticleen_US

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