Sequence Stratigraphic, Facies &amp; Reservoir Framework for the Bangestan Group, Lurestan, Zagros Mountains, Iran

Sharp, Ian; Embry, J.C.; Hunt, Dave; Morsalnezhad, D.; Packer, Stephen; Caus, Esmeralda; Jalili, M.; Bang, Nils; Keyvani, Forooz; Livbjerg, F.; Lønøy, A.; Samuelsberg, Tommy J.; Dons, Carl E.

doi:10.3997/2214-4609.20145342

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Sequence Boundaries2

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2016

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“…Sharp et al (2010) identified three regionally extensive karst surfaces in the uppermost Cenomanian-Turonian interval, and interpreted them to be related to flexure of the Arabian Plate margin due to the initiation of intra-oceanic deformation. The first of these karst surfaces (their Sb-Sa4) is the Cenomanian/Turonian boundary, which caps a strongly progradational Mishrif Formation.…”

Section: Sequence Boundariesmentioning

confidence: 99%

“…The first of these karst surfaces (their Sb-Sa4) is the Cenomanian/Turonian boundary, which caps a strongly progradational Mishrif Formation. Above the first karst surface, Sharp et al (2010) reported that the lower Turonian sequence (their Sa5 sequence) is typically missing due to truncation by a second karst surface (their Sb-Sa5). The middle and upper Turonian sequence (their Sa-6) is capped by a third karst surface (their Sb-Sa6) and is overlain by the Coniacian Surgah Formation.…”

Section: Sequence Boundariesmentioning

confidence: 99%

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