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- W2187955455 abstract "Ten depositional shoalingcycles have been identified in the Aptian Shuaiba Formation of theUnited Arab Emirates U A similar numberof cycles havebeen recognized intheNational Petroleum Reserve of Alaska NPRASimilarities of these cycles with the onlapping shelf geometries of the Neogene of theBahamas suggest that the sequence geometries of Aptian strata of the NPRA and theU are a response tohigh changes in eustatic sea position Because the Aptian cycles of the NPRA match similarly dated events in theU it is suggested that where biostratigraphic data are poor thesedimentary section canbe tentatively dated by relating the geometries of the shelf margin to the character of thecoastal onlap curve and its coincident sea chart Thus a sea chart might be used at locations for whichbiostratigraphic data is sparse to determine and constrain preliminary depositional models for specific time intervals With thisin mind two biostratigraphic models for dating the Shuaiba Formation and the Bab Member weretested against thesea curve of Haq et al1987 using asedimentary simulation The resultswereambiguous becauseboth biostratigraphic models could notbe matched Also inboth cases thesimulation suggested that just prior to the deposition of the Bab Member the basinmargin was uplifted and then subsided causing a local relative sea fall followed by a rise an event notfound on thesea chart of Haq et al1987 Additionally the sedimentary simulation supports the position that the Aptian in theU is bounded by erosional unconformity surfaces and containshigher cycles" @default.
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- W2187955455 date "2012-01-01" @default.
- W2187955455 modified "2023-09-26" @default.
- W2187955455 title "CAN THE SEDIMENTARY RECORD BE DATED FROM A SEA CHART EXAMPLES FROM THE APTIAN OF THEU AND ALASKA" @default.
- W2187955455 hasPublicationYear "2012" @default.
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