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Abstract

New biostratigraphic interpretations have provided a basis for identifying fourth-order cycles within the Mishrif Member, and can be tied to log and seismic data, allowing construction of chronostratigraphic lithofacies maps. Higher-frequency depositional cyclicity is also observed, and it is possible to interpret individual geobodies in areas with 3D seismic coverage and well control.

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/content/papers/10.3997/2214-4609.20145352
2010-01-24
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20145352
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