SPE EUROPEC/EAGE Annual Conference and Exhibition 2010
DOI: 10.2118/130786-ms
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Multidisciplinary Workflow applied to Multiple Stage Hydraulic Fracturing of Horizontal Wellbores: Evolving the Process in the Lebada Field, Black Sea

Abstract: Oil production from offshore Lebada field has been improved significantly over the last two years through the use of multiple proppant fractures placed from horizontal completions. Following early successes the engineering effort now focuses on increasing value through engineering innovation and increased productivity. This paper describes, through case histories and field data, the advances made in the application of workflow processes, design and execution of these completions. Due to the offs… Show more

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Cited by 3 publications
(2 citation statements)
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“…The Upper Cretaceous reservoir is a calcareous, post-rift sequence also known as the Santonian-Coniacian-Turonian complex (St-Co-Tu complex). It is a micro-fractured reservoir complex with a mixed carbonate and sandstone lithology (Cațaraiani et al, 2010;Contreras and Sarmiento, 2016). Occasional conglomerates and calcareous-sandstone layers are present at the bottom of the section ranging from 10 to 20 cm thickness up to 5-10 m. At the middle of the section, calcareous-sands and marl intervals overlain by a 30-35 m thick micritic-biogenic-limestone cap-rock dominate the mixture.…”
Section: Geological Setting and Stratigraphymentioning
confidence: 99%
See 1 more Smart Citation
“…The Upper Cretaceous reservoir is a calcareous, post-rift sequence also known as the Santonian-Coniacian-Turonian complex (St-Co-Tu complex). It is a micro-fractured reservoir complex with a mixed carbonate and sandstone lithology (Cațaraiani et al, 2010;Contreras and Sarmiento, 2016). Occasional conglomerates and calcareous-sandstone layers are present at the bottom of the section ranging from 10 to 20 cm thickness up to 5-10 m. At the middle of the section, calcareous-sands and marl intervals overlain by a 30-35 m thick micritic-biogenic-limestone cap-rock dominate the mixture.…”
Section: Geological Setting and Stratigraphymentioning
confidence: 99%
“…Occasional conglomerates and calcareous-sandstone layers are present at the bottom of the section ranging from 10 to 20 cm thickness up to 5-10 m. At the middle of the section, calcareous-sands and marl intervals overlain by a 30-35 m thick micritic-biogenic-limestone cap-rock dominate the mixture. The targets consist of a thin laminated and tight reservoir with porosity values from 0% up to 25% while permeability ranges from 0.1 to 2.0 mD with an average of 0.8 mD (Bukovac et al, 2009;Cațaraiani et al, 2010;Sofonea et al, 1996).…”
Section: Geological Setting and Stratigraphymentioning
confidence: 99%