Depositional Environment of Lidam and Nubian Sanstone
Miloud M. Abugares
Abstract
Miloud M. Abugares
Abstract
P054 DEPOSITIONAL ENVIRONMENT OF LIDAM AND NUBIAN SANSTONE Abstract 1 The sedimentary sequence infilling Sirt basin was initiated by Nubian Sandstone which is separated from underlying granitic by the Hercynian unconformity and the upper boundary of the sequence by another unconformity followed by an early Late Cretaceous transgressive lithofacies of Lidam Formation. The Nubian sandstone sequence penetrated in the studied well 3V1-59W are 449 ft thickness from depth10546 ft to 10995 ft) of which 106 feet gap and the upper part in is Lidam formation (Cenomnain age) which considered the reservoir for hydrocarbon in concession 59 East 3V-59 block. The
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P054 DEPOSITIONAL ENVIRONMENT OF LIDAM AND NUBIAN SANSTONE Abstract 1 The sedimentary sequence infilling Sirt basin was initiated by Nubian Sandstone which is separated from underlying granitic by the Hercynian unconformity and the upper boundary of the sequence by another unconformity followed by an early Late Cretaceous transgressive lithofacies of Lidam Formation. The Nubian sandstone sequence penetrated in the studied well 3V1-59W are 449 ft thickness from depth10546 ft to 10995 ft) of which 106 feet gap and the upper part in is Lidam formation (Cenomnain age) which considered the reservoir for hydrocarbon in concession 59 East 3V-59 block. The
Key concepts: Unconformity, Sedimentary depositional environment, Geology, Sequence (biology), Cretaceous, Sedimentary rock, Structural basin, Paleontology