Day 1 Tue, January 24, 2017 2017
DOI: 10.2118/184823-ms
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From the Backyard Dune to Fracturing a Highly Tectonically Complex Formation in Saudi Arabia

Abstract: Sand in Saudi Arabia is easily accessible through surface mining or excavating large dunes that are API approved, but like many sands around the world, lacks the necessary strength for fracturing high stress formations. To exploit the sand, a novel engineered workflow, enabled by the flow channel fracturing technique was established for qualifying and implementing Saudi Arabian sand to fracture stimulate the tectonically complex ultra-tight "T" carbonate formation. Channel fracturing does not de… Show more

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Cited by 9 publications
(4 citation statements)
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“…Horizontal bedding planes, mechanically weak owing to little cohesion, may be stimulated in shale plays in transitional strike-slip to reverse faulting stress regimes, in which S v and S hmin are close in magnitudes and similar to the least principal stress (i.e., S hmin ∼S v ∼S 3 ). Such stress conditions have been reported in some unconventional source rock plays (e.g., the Marcellus Shale in southern West Virginia and the Tuwaiq Mountain formation in the Jafurah Basin, Saudi Arabia [27,38,39]).…”
Section: Third Fracture Scenario: Vertical Hydraulic Fractures With Horizontal Bedding Plane Fracturessupporting
confidence: 60%
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“…Horizontal bedding planes, mechanically weak owing to little cohesion, may be stimulated in shale plays in transitional strike-slip to reverse faulting stress regimes, in which S v and S hmin are close in magnitudes and similar to the least principal stress (i.e., S hmin ∼S v ∼S 3 ). Such stress conditions have been reported in some unconventional source rock plays (e.g., the Marcellus Shale in southern West Virginia and the Tuwaiq Mountain formation in the Jafurah Basin, Saudi Arabia [27,38,39]).…”
Section: Third Fracture Scenario: Vertical Hydraulic Fractures With Horizontal Bedding Plane Fracturessupporting
confidence: 60%
“…Some mudrock plays are further characterized by high pore pressure and a small difference between the principal stresses. For example, the Jafurah basin exhibits pore pressure gradients between 0.016 and 0.020 MPa/m (∼0.7-0.88 psi/ft) [38,44], and strike-slip faulting stress regime (S hmin ∼0.96 psi/ft < S v ∼ 1.1 psi/ft < S Hmax ∼1.2 psi/ft) [38,44,82]. These environments combined with large fluid volume injection foster interactions between vertical hydraulic fractures and pre-existing discontinuities (e.g., natural fractures and bedding planes).…”
Section: Resultsmentioning
confidence: 99%
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