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dc.contributor.authorAl-Ghamdi, Nasser Mohammaden_US
dc.date.accessioned2014-03-14T20:38:34Z
dc.date.available2014-03-14T20:38:34Z
dc.date.issued2006-05-19en_US
dc.identifier.otheretd-05252006-150116en_US
dc.identifier.urihttp://hdl.handle.net/10919/33225
dc.description.abstractThe Cretaceous (Early Aptian) Shu'aiba Formation, Shaybah field, Saudi Arabia, is 60 km long by 12 km wide and 150 m thick, and is a giant carbonate reservoir. It formed on a regional carbonate ramp bordering an intrashelf basin. The succession consists of a composite sequence of seven high frequency sequences. Sequences 1 and 2 formed a deeper open platform of Palorbitolina-Lithocodium wackestone, with maximum flooding marked by planktic foram mudstone. Sequence 2 built relief over northern and southern blocks, separated by an intraplatform depression. They form the composite sequence TST. The remaining sequences developed a platform rimmed by rudist rudstone backed by rudist floatstone back-bank and lagoonal fine skeletal peloidal packstone; slope facies are fine skeletal fragmented packstone. Aggradational sequences 3 to 5 make up the composite sequence early highstand. Progradational sequences 6 and 7 are the composite sequence late highstand marking the deterioration of the Offneria rudist barrier and deposition of widespread lagoonal deposits, where accommodation may have been created by syn-depositional growth faulting that moved the northern block down. Shu'aiba deposition on the platform was terminated by long-term sea-level fall and karsting.

The succession is dominated by approximately 400 k.y., 4th order sequences and 100 k.y. parasequences driven by long term eccentricity and short term eccentricity respectively, similar to the Pacific guyots of this age. This suggests that early Cretaceous climate may have been cooler and had small ice sheets and was not an ice-free greenhouse world.

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dc.publisherVirginia Techen_US
dc.relation.haspartCompleteShuaibaThesis.pdfen_US
dc.rightsI hereby certify that, if appropriate, I have obtained and attached hereto a written permission statement from the owner(s) of each third party copyrighted matter to be included in my thesis, dissertation, or project report, allowing distribution as specified below. I certify that the version I submitted is the same as that approved by my advisory committee. I hereby grant to Virginia Tech or its agents the non-exclusive license to archive and make accessible, under the conditions specified below, my thesis, dissertation, or project report in whole or in part in all forms of media, now or hereafter known. I retain all other ownership rights to the copyright of the thesis, dissertation or project report. I also retain the right to use in future works (such as articles or books) all or part of this thesis, dissertation, or project report.en_US
dc.subjectSequence Frameworken_US
dc.subjectShu'aiba Formationen_US
dc.subjectSaudi Arabiaen_US
dc.subjectFaciesen_US
dc.subjectand Evolution of Rudist Buildupsen_US
dc.titleFacies, Sequence Framework, and Evolution of Rudist Buildups, Shu'aiba Formation, Saudi Arabiaen_US
dc.typeThesisen_US
dc.contributor.departmentGeosciencesen_US
dc.description.degreeMaster of Scienceen_US
thesis.degree.nameMaster of Scienceen_US
thesis.degree.levelmastersen_US
thesis.degree.grantorVirginia Polytechnic Institute and State Universityen_US
thesis.degree.disciplineGeosciencesen_US
dc.contributor.committeechairRead, James Fredricken_US
dc.contributor.committeememberLaw, Richard D.en_US
dc.contributor.committeememberEriksson, Kenneth A.en_US
dc.identifier.sourceurlhttp://scholar.lib.vt.edu/theses/available/etd-05252006-150116/en_US
dc.date.sdate2006-05-25en_US
dc.date.rdate2007-06-15
dc.date.adate2006-06-12en_US


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