Salt Control on Sedimentary Processes in Early Pleistocene: Ship Shoal South Addition Blocks 349-358, Gulf of Mexico.

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dc.contributor.advisor Watkins , Joel S . en_US
dc.contributor.committeeMember Ayers , Walter B . en_US
dc.creator Syarif , Munji en_US
dc.date.accessioned 2004 -09 -30T02 :07 :20Z
dc.date.accessioned 2014 -02 -19T18 :30 :32Z
dc.date.available 2004 -09 -30T02 :07 :20Z
dc.date.available 2014 -02 -19T18 :30 :32Z
dc.date.created 2002 -12 en_US
dc.date.issued 2004 -09 -30T02 :07 :20Z
dc.identifier.uri http : / /hdl .handle .net /1969 .1 /517
dc.description.abstract The interpretation of 3D seismic data from Ship Shoal South Addition Blocks 349 -358 , Gulf of Mexico shows a complex interaction between salt , faults , and sedimentary strata . Reconstruction of the geometry of early Pliestocene (about 3 .65 Ma ) through recent salt and associated sediments reveals the evolution of a supralobal basin in the study area . The basin depocenter shifted from the northeastern part to the center of the study area through time . A small , bulb -shaped , salt -stock structure occurs in the northwest , and a salt sheet structure is present in the southeastern part of the study area . Those structures are part of a pennant -shaped structure bounded by counter regional faults trending northeastward . Salt movements created instability and triggered extensive faulting of the overlying strata . Three -dimensional reconstruction suggests that salt blocked the sediment during the early Pleistocene . The sediment was diverted around the salt high on both east and west sides of the salt body to the southwest and southeast . Stratigraphic interpretation of the interval between 1 .35 Ma and 1 .95 Ma led to the identification of a highstand systems tract (HST ) , a transgressive systems tract (TST ) , and two lowstand systems tracts (LST ) . The strata are developed normally in the depocenter area , whereas the strata at the basin margin were deformed by salt movement and faulting . Each systems tract is uniquely associated with a certain seismic facies . Three seismic facies were identified associated with LST , TST , and HST . Additionally , seismic sections reveal channel geometries in the LST . Seismic attribute analysis elucidates facies distribution in the systems tracts . Because of its ability to move , to divert sediment , to create instability , and to block sediment transport pathways , salt exercises the main control on the sedimentary processes in the study area . en_US
dc.format.extent 42764591 bytes
dc.format.medium electronic en_US
dc.format.mimetype application /pdf
dc.language.iso en _US en_US
dc.publisher Texas A &M University en_US
dc.rights I 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 Texas A &M University 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.subject salt tectonics en_US
dc.title Salt Control on Sedimentary Processes in Early Pleistocene : Ship Shoal South Addition Blocks 349 -358 , Gulf of Mexico . en_US
dc.type Book en
dc.type.genre Electronic Thesis en_US
dc.type.material text en_US
dc.format.digitalOrigin born digital en_US

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Salt Control on Sedimentary Processes in Early Pleistocene: Ship Shoal South Addition Blocks 349-358, Gulf of Mexico.. Available electronically from http : / /hdl .handle .net /1969 .1 /517 .

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