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Dissertations / Theses on the topic 'Sequence stratigraphy'

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Published: 4 June 2021

Last updated: 25 July 2025

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1

Nakanishi, Takeshi. "Practical application of sequence stratigraphy and risk analysis for stratigraphic trap exploration." Title page, contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09PH/09phn1635.pdf.

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"September 2002" Includes bibliographical references (leaves 200-209) Outlines an evaluation procedure for stratigraphic trap exploration by employing sequence stratigraphy, 3D seismic data visualisation and quantitative risk analysis with case studies in an actual exploration basin.

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2

Kahmann-Robinson, Julia A. Atchley Stacy C. "The sequence stratigraphic evolution of the Sturgeon Lake bank, central Alberta, Canada and its regional implications." Waco, Tex. : Baylor University, 2005. http://hdl.handle.net/2104/3016.

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3

Nunes, Caio Oliveira. "Tectonic and stratigraphic evolution of southern Jacuípe basin based on seismic sequence stratigraphy." IGEO, 2018. http://repositorio.ufba.br/ri/handle/ri/26188.

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Submitted by Everaldo Pereira (pereira.evera@gmail.com) on 2018-05-27T13:07:21Z No. of bitstreams: 1 Caio Dissertação Mestrado (Versão FINAL).pdf: 6456975 bytes, checksum: cb47f45f811eedcbb8b5288fd76f3f06 (MD5)<br>Approved for entry into archive by NUBIA OLIVEIRA (nubia.marilia@ufba.br) on 2018-06-18T18:15:34Z (GMT) No. of bitstreams: 1 Caio Dissertação Mestrado (Versão FINAL).pdf: 6456975 bytes, checksum: cb47f45f811eedcbb8b5288fd76f3f06 (MD5)<br>Made available in DSpace on 2018-06-18T18:15:34Z (GMT). No. of bitstreams: 1 Caio Dissertação Mestrado (Versão FINAL).pdf: 6456975 bytes, checks

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4

Shelton, Jessica Anne. "Application of sequence stratigraphy to the nonmarine Upper Cretaceous Two Medicine Formation, Willow Creek anticline, northwestern, Montana." Thesis, Montana State University, 2007. http://etd.lib.montana.edu/etd/2007/shelton/SheltonJ0507.pdf.

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5

Suchy, Daniel R. "Hudson Bay platform : silurian sequence stratigraphy and paleoenvironments." Thesis, McGill University, 1992. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=70280.

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Trends in relative sea-level change, shown by curves drawn from drill core and outcrop sections in Llandoverian carbonates of the Hudson Bay Platform, were used to correlate individual parasequences among widely separated localities. Two sequences, bounded by regional disconformities, include: (1) the Severn River Formation, and (2) the Ekwan River, Attawapiskat, and Kenogami River Formations. Initial onlap of marine facies at the base of the Severn River Formation progressed from north to south, occurring first in the Hudson Bay Basin, then in the Moose River Basin; final retreat of the seas

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6

Al, Kharusi Laiyyan Mohammed. "Correlation between High Resolution Sequence Stratigraphy and Mechanical Stratigraphy for Enhanced Fracture Characteristic Prediction." Scholarly Repository, 2009. http://scholarlyrepository.miami.edu/oa_dissertations/339.

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Sequence stratigraphy relates changes in vertical and lateral facies distribution to relative changes in sea level. These relative changes in carbonates effect early diagenesis, types of pores, cementation and dissolution patterns. As a result, in carbonates, relative changes in sea level significantly impact the lithology, porosity, diagenesis, bed and bounding surfaces which are all factors that control fracture patterns. This study explores these relationships by integrating stratigraphy with fracture analysis and petrophysical properties. A special focus is given to the relationship betwee

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7

Stubbs, Dreadnaught G. "A Sequence Stratigraphic Analysis of the Allegheny Group (Middle Pennsylvanian),Southeast Ohio." Ohio University / OhioLINK, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1524600396756809.

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8

Demirel, Seda. "Foraminiferal Paleontology And Sequence Stratigraphy In The Upper Visean." Master's thesis, METU, 2012. http://etd.lib.metu.edu.tr/upload/12614831/index.pdf.

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The aim of this study is to investigate the Upper Visean substages, delineate the Visean - Serpukhovian boundary with calcareous foraminifera and interpret the foraminiferal evolution and sequence stratigraphical framework by using sedimentary cyclicity across the boundary section. For this purpose a 59,61 m thick stratigraphic section consisting of mainly limestone and partly sandstone and shale is measured in the Aziziye Gedigi and Oru&ccedil<br>oglu Formations in the Pinarbasi Region of Eastern Taurides. A detailed micropaleontological study has revealed presence of important foraminifera

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9

Owoyemi, Ajibola Olaoluwa. "Sequence stratigraphy of Niger Delta, Delta field, offshore Nigeria." Texas A&M University, 2004. http://hdl.handle.net/1969.1/2768.

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The Niger Delta clastic wedge formed along the West Africa passive margin. This wedge has been divided into three formations that reflect long-term progradation: 1) pro-delta shales of the Akata Formation (Paleocene to Recent), 2) deltaic and paralic facies of the Agbada Formation (Eocene to Recent) and 3) fluviatile facies of the Benin Formation (Oligocene-Recent). This study combines a three-dimensional seismic image with well log data from Delta field to describe lithic variations of the Agbada Formation and develop a sequence stratigraphic framework. The 5000-feet thick Agbada Formation in

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10

Magbagbeola, Olusola Akintayo. "Sequence stratigraphy of Niger Delta, Robertkiri field, onshore Nigeria." Texas A&M University, 2005. http://hdl.handle.net/1969.1/4768.

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Deposits of Robertkiri field, in the central offshore area of Niger Delta, comprise a 4 km thick succession of Pliocene to Miocene non-marine and shallow marine deposits. A sequence stratigraphic framework for Robertkiri field strata was constructed by combining data from 20 well logs and a seismic volume spanning 1400 km2. Major sequences, hundreds of meters thick, define layers of reservoir and sealing strata formed during episodic progradation and retrogradation of deltaic shorelines. These deposits progress upward from fine-grained prodelta and deep water shales of the Akata Formation thro

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11

Ardill, John. "Sequence stratigraphy of the Mesozoic Domeyko basin, northern Chile." Thesis, University of Liverpool, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.307620.

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The Domeyko basin of northern Chile records Late Triassic-Early Cretaceous mixed carbonate and siliciclastic marine deposition along the western margin of Gondwana. The carbonate and siliciclastic ramp environment is characterised by the deposition of siliciclastic-dominated sediments at times of low accommodation space (lowstand and late highstand systems tracts) and carbonate-dominated sediments during periods of high accommodation space (transgressive and early highstand systems tracts). Along strike variations in siliciclastic sediment supply do not overprint the effects of basinwide chang

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12

Salem, Yahya Ahmed Ali. "Sequence stratigraphy of the Palaeozoic Ghadamis Basin NW Libya." Thesis, University of Birmingham, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.420859.

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13

Udgata, Devi Bhagabati Prasad. "Glauconite as an indicator of sequence stratigraphic packages in a Lower Paleocene passive-margin shelf succession, Central Alabama." Auburn, Ala., 2007. http://repo.lib.auburn.edu/07M%20Theses/UDGATA_DEVI_55.pdf.

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14

Shoore, David Joseph. "Sequence stratigraphy of the Bridal Veil Falls Limestone, carboniferous, Oquirrh Group, on Cascade Mountain, Utah : a standard Morrowan cyclostratigraphy for the Oquirrh basin /." Diss., CLICK HERE for online access, 2004. http://contentdm.lib.byu.edu/ETD/image/etd775.pdf.

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15

Robinson, Eric D. "Facies architecture of the Upper Sego member of the Mancos Shale Formation, Book Cliffs, Utah." Texas A&M University, 2005. http://hdl.handle.net/1969.1/3270.

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The Late Cretaceous upper Sego Member of the Mancos Shale exposed in the Book Cliffs of east-central Utah is a 30 m thick sandstone wedge that overlies the Anchor Mine Tongue of the Mancos Shale and underlies coastal plain deposits of the Neslen Formation. Although this sandstone has been interpreted to be comprised of transgressive valley fills, recent detailed facies architecture studies of the underlying lower Sego Sandstone suggest these deposits may instead be regressive deposits of tideinfluenced deltas. This study maps facies associations, the geometry of lithic bodies, and key stratigr

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16

Badescu, Adrian Constantin. "Reservoir characterization of the Miocene Starfak and Tiger Shoal fields, offshore Louisiana through integration of sequence stratigraphy, 3-D seismic, and well-log data." Access restricted to users with UT Austin EID, 2002. http://wwwlib.umi.com/cr/utexas/fullcit?p3108452.

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17

Bowman, Andrew Philip. "Sequence stratigraphy and reservoir characterisation in the Columbus Basin, Trinidad." Thesis, Imperial College London, 2004. http://hdl.handle.net/10044/1/7990.

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18

Parkinson, D. Neil. "The sequence stratigraphy of the Lower Jurassic of Western Europe." Thesis, University of Oxford, 1994. http://ora.ox.ac.uk/objects/uuid:cddbc521-f687-41dd-a9ad-f70621012555.

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The Lower Jurassic stratigraphy of seven contrasting areas in western Europe is compared in order to seek evidence for a pan-Western European stratigraphic forcing mechanism. Sequencestratigraphic models are discussed and emphasis is placed upon the differing response of sedimentary systems in "accommodation space-dominated" and "supply-dominated" settings. Spectral gamma-ray data from clastic successions in the Wessex and Cleveland basins (England) are used to elucidate vertical trends. A proximal-distal model for control of Th/K ratios is advanced. Stage-frequency regressive-transgressive cy

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19

Ahmadi, Ziad M. "Sequence stratigraphy using wireline logs from Upper Jurassic of England." Thesis, Durham University, 1997. http://etheses.dur.ac.uk/1644/.

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20

Smith, Tyson Bartek Louis Robert. "Sequence stratigraphy and stratigraphic architecture of the upper Mississippian lower Hinton Formation Appalachian Basin, West Virginia, USA /." Chapel Hill, N.C. : University of North Carolina at Chapel Hill, 2009. http://dc.lib.unc.edu/u?/etd,2651.

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Thesis (M.S.)--University of North Carolina at Chapel Hill, 2009.<br>Title from electronic title page (viewed Oct. 5, 2009). "... in partial fulfillment of requirements for the degree of Master's of Geological Sciences in the Department of Geological Sciences." Discipline: Geology; Department/School: Geological Sciences.

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21

Cleveland, David M. Atchley Stacy C. Nordt Lee C. "Fluvial sequence stratigraphy and paleoclimate of the Upper Triassic (Norian-Rhaetian) Chinle Strata, northern New Mexico." Waco, Tex. : Baylor University, 2007. http://hdl.handle.net/2104/5118.

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Thesis (Ph.D.)--Baylor University, 2007.<br>In the abstract "[delta]13C" the "13" and "[delta]18O" the "18" are superscript; "pCO2" the "2" is subscript. Includes bibliographical references (p. 107-118).

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22

Eifert, Tambra L. "The Cretaceous-Paleogene transition in the northern Mississippi Embayment, S.E. Missouri: palynology, micropaleontology, and evidence of a mega-tsunami deposit." Diss., Rolla, Mo. : Missouri University of Science and Technology, 2009. http://scholarsmine.mst.edu/thesis/pdf/Eifert_09007dcc80658622.pdf.

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Thesis (Ph. D.)--Missouri University of Science and Technology, 2009.<br>Vita. The entire thesis text is included in file. Title from title screen of thesis/dissertation PDF file (viewed May 4, 2009) Includes bibliographical references (p. 243-265).

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23

McLaughlin, Patrick I. "Cratonic sequence stratigraphy advances from analysis of mixed carbonate-siliciclastic successions /." Cincinnati, Ohio : University of Cincinnati, 2006. http://www.ohiolink.edu/etd/view.cgi?acc%5Fnum=ucin1147959013.

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Thesis (Ph. D.)--University of Cincinnati, 2006.<br>Title from electronic thesis title page (viewed Aug. 3, 2006). Includes abstract. Keywords: faunal gradient analysis, taphonomy, hardground, condensed bed, cyclothem, Lexington Limestone, Paleozoic, forced regression. Includes bibliographical references.

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24

Hall, Matthew Thomas. "Sequence stratigraphy and early diagenesis : the Sobrarbe Formation, Ainsa Basin, Spain." Thesis, University of Manchester, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.516716.

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25

Oliver, Guy Mark. "High-resolution sequence stratigraphy and diagenesis of mixed carbonate/siliciclastic successions." Thesis, University of Plymouth, 1997. http://hdl.handle.net/10026.1/2019.

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The aims of this thesis are to evaluate whether the distribution of diagenetic features in nearshore successions can be explained within a sequence stratigraphic concept; to assess whether the identification and analysis of these features can be used to aid in making sequence stratigraphic interpretations; and to evaluate whether sequence stratigraphy can be used to predict the distribution of diagenetic heterogeneities at the field and inter-well scale. High resolution sequence stratigraphic frameworks have been established for two nearshore mixed carbonate/siliciclastic successions, using fa

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26

McLAUGHLIN, PATRICK I. "CRATONIC SEQUENCE STRATIGRAPHY: ADVANCES FROM ANALYSIS OF MIXED CARBONATE-SILICICLASTIC SUCCESSIONS." University of Cincinnati / OhioLINK, 2006. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1147959013.

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27

Pierson, Jessica A. "Late cretaceous (Campanian and Maastrichtian) sequence stratigraphy, southeastern North Carolina, USA /." Electronic version (PDF), 2003. http://dl.uncw.edu/etd/2003/piersonj/jessicapierson.pdf.

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28

Maxwell, Gregor. "The sedimentology and sequence stratigraphy of the Middle Jurassic Beryl Formation, Quad 9, U.K.C.S." Thesis, University of Aberdeen, 1999. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=236949.

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Quad 9 of the U.K.C.S., North Sea is located 215 miles NE of Aberdeen. It contains four producing fields with over 400 mmbbls of oil and NGL's and 5.1 TCF of gas initially in place. The major reservoir unit is the Middle Jurassic (Bajocian to Bathonian) Beryl Formation, a marginal to shallow marine deposit which varies in thickness from 150' to 1100' across the studied area. It was deposited within the Beryl Embayment, a transfer zone between two actively extending basin bounding faults of the South Viking Graben, prior to the onset of the major rifting phase during the Callovian to Ryazanian.

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29

Kells, Melanie P. "Sequence stratigraphy and depositional history of the Artinskian to Kungurian sequence, Otto Fiord area, northwestern Ellesmere Island." Thesis, University of Ottawa (Canada), 1996. http://hdl.handle.net/10393/10139.

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The Artinskian to Kungurian Sequence of the Otto Fiord area is dominated by the Great Bear Cape, Raanes and Trappers Cove formations in addition to the upper portions of the Nansen and Hare Fiord formations. The Great Bear Cape Formation (10-300 m), in the Otto Fiord area, is a yellowish-weathering, cliff-forming, packstone to grainstone dominated by echinoderms, bryozoans, and brachiopods. The Raanes Formation (10-225 m) is greenish-weathering, recessive to resistant, shaly to silty, variably cherty wackestone to packstone dominated by bryozoans, brachiopods, crinoids, and sponge spicules in

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30

Gollop, Alison. "Structural controls on the seismic sequence stratigraphy of the Ben Nevis, Avalon, and Eastern Shoals formations, Terra Nova field, Jeanne D'Arc Basin, offshore Newfoundland /." Internet access available to MUN users only, 2003. http://collections.mun.ca/u?/theses,76559.

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31

Isnard, Hélène. "Application des traceurs isotopiques Pb-Pb, Sm-Nd et Lu-Hf à la compréhension de l'histoire archéenne du bouclier canadien et à la formation de la croûte continentale /." Thèse, Chicoutimi : Montréal : Université du Québec à Chicoutimi ;. Université du Québec à Montréal, 2003. http://theses.uqac.ca.

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Thèse (D.R.Min.) -- Université du Québec à Chicoutimi, programme extensionné à l'Université du Québec à Montréal, 2003.<br>Bibliogr.: f. 203-204. Document électronique également accessible en format PDF. CaQCU

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32

BARTHOLOMEW, ALEXANDER. "CORRELATION OF HIGH ORDER CYCLES IN THE MARINE-PARALIC TRANSITION OF THE UPPER MIDDLE DEVONIAN (GIVETIAN) MOSCOW FORMATION, EASTERN NEW YORK STATE." University of Cincinnati / OhioLINK, 2002. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1022593337.

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33

Cavas, Matthew P. "THE QUATERNARY GEOLOGY AND SEQUENCE STRATIGRAPHY OF THE LAKE BONNEVILLE DEPOSITS IN THE MATLIN QUADRANGLE, BOX ELDER COUNTY, NORTHWESTERN UTAH." Ohio University / OhioLINK, 2003. http://www.ohiolink.edu/etd/view.cgi?ohiou1080586528.

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34

Campo, Bruno <1984&gt. "The Pleistocene-Holocene Transition in the Po Plain (Italy): Stratigraphic Architecture and Sequence Stratigraphy from a Highly-Subsiding Basin." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amsdottorato.unibo.it/7540/1/Tesi_dottorato_XXVIII_ciclo_Bruno_Campo_Esame_Finale_2016.pdf.

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This work focuses on the Late Pleistocene-Holocene transition in the southern Po Basin. Five areas were investigated, with the aim of unraveling the role of different allogenic factors (climate, eustacy, sediment supply) on stratigraphic architecture in the last 45 ky. The study starts from the distal portion of the basin (the coastal plain deposits) and then moves towards increasingly internal areas: the alluvial sector characterized by the Po channel belt deposits, and the mud-prone interfluvial succession between the Apenninic margin and the Po channel belt. In the coastal sector, high-reso

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35

Campo, Bruno <1984&gt. "The Pleistocene-Holocene Transition in the Po Plain (Italy): Stratigraphic Architecture and Sequence Stratigraphy from a Highly-Subsiding Basin." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amsdottorato.unibo.it/7540/.

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This work focuses on the Late Pleistocene-Holocene transition in the southern Po Basin. Five areas were investigated, with the aim of unraveling the role of different allogenic factors (climate, eustacy, sediment supply) on stratigraphic architecture in the last 45 ky. The study starts from the distal portion of the basin (the coastal plain deposits) and then moves towards increasingly internal areas: the alluvial sector characterized by the Po channel belt deposits, and the mud-prone interfluvial succession between the Apenninic margin and the Po channel belt. In the coastal sector, high-reso

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36

Al-Mojel, Abdullah. "Sedimentology and sequence stratigraphy of the Jurassic, Jabal Tuwaiq, Central Saudi Arabia." Thesis, Bordeaux 3, 2017. http://www.theses.fr/2017BOR30037/document.

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Cette étude porte sur l’analyse des séries jurassiques du Shaqra Group (Toarcian to Kimmeridgian) qui affleurent de manière continue en Arabie centrale le long d’un transect de plus de 1000 km de long. Ces séries se sont accumulées sur une vaste plate-forme épicontinentale peu profonde, en contexte tropical. Ces affleurements permettent ainsi d’observer la partie occidentale des séries renfermant des systèmes pétroliers prolifiques exploités en subsurface en Arabie Saoudite. L’analyse sédimentologique de nombreuses coupes et la réalisation de corrélations stratigraphiques de haute résolution s

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37

Best, Heidi Ann. "Sedimentology, sequence stratigraphy and reservoir potential of the Warrinilla Field, Bowen Basin /." Title page, contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bb561.pdf.

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38

Ceglar, Nathan. "Late Jurassic to Early Cretaceous sequence stratigraphy, Northern Bonaparte Basin, Timor Sea /." Title page, contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09SB/09sbc389.pdf.

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39

Faulkner, Tony. "Sequence stratigraphy of the Late Cretaceous Sherbook group, Shipwreck Trough, Otway Basin /." Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bf263.pdf.

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40

Sher, Mohammad. "Seismic interpretation and sequence stratigraphy of the offshore indus basin of Pakistan." Thesis, Oxford Brookes University, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.326205.

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41

Wonham, Jonathan Philip. "Sedimentology and sequence stratigraphy of tidal sandstone bodies : implications for reservoir characterisation." Thesis, University of Liverpool, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.240411.

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Analysis of the facies and sequence stratigraphy of tidally-influenced, siliciclastic-dominated successions from five different areas has allowed a survey and comparison of the sedimentological and architectural characteristics of a variety of tidal sandstone body types. This study is concerned with: (i) describing these different sandstone body types; (ii) analysing the controls on sandstone body internal architecture, external geometry and connectivity, and (iii) outlining the implications of such studies for reservoir characterisation. Facies analysis of the studied successions by previous

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42

Couzens, Timothy John. "The rift to drift transition and sequence stratigraphy at passive continental margins." Thesis, University of Liverpool, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.333509.

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Most passive margins display a prominent breakup unconformity coinciding with the rift to drift transition. The unconformity, as defined by Falvey, (1974) is of broad regional extent affecting both basins and highs and is easily recognised on seismic sections. Criteria for the recognition of the breakup unconformity include an inflection in the subsidence curve, fault terminations and volcanic strata (and/or evaporites) at the level of the unconformity. Falvey considered that it was caused by "erosion during the final uplift pulse associated with pre-breakup upwelling in the mantle". It is mor

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43

Dayley, Jason. "Nonmarine Sequence Stratigraphy of the Gannett Group Southeastern Idaho and Western Wyoming." Thesis, University of Louisiana at Lafayette, 2016. http://pqdtopen.proquest.com/#viewpdf?dispub=10002483.

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<p> Late Jurassic through Early Cretaceous strata of the Gannett Group record initial development of the Sevier thrust belt and adjacent foreland basin. Concepts of nonmarine sequence stratigraphy were used to determine the depositional and base level history of the Gannett Group in southeastern Idaho and western Wyoming. Base level fluctuations were driven entirely by tectonic processes, while tectonic uplift in the source area was a major control on sequence development. Six measured sections were revisited or measured and correlated using the concepts of sequence stratigraphy. Four distinct

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44

Menegatti, Alessandra. "Biostratigraphy, sedimentology and high resolution sequence stratigraphy of the Mishrif Formation, Dubai." Thesis, University of Aberdeen, 2004. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=228967.

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The Middle to Upper Cenomanian Mishrif Formation of Dubai has been interpreted applying biostratigraphic, sedimentologic and sequence stratigraphic concepts. Fourteen wells have been analysed in core and thin-section. These key wells were chosen to cover the geographical extent of the Mishrif and its stratigraphic distribution in offshore Dubai. The identification of thirteen biofacies is based on the trends In composition of microfossil assemblages. Observations on sedimentary features, both in core and thinsection, were also made. Six age significant bioevents are used to constrain stratigra

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45

Al-Tawil, Aus. "High resolution sequence stratigraphy of late Mississippian carbonates in the Appalachian Basin." Diss., Virginia Tech, 1998. http://hdl.handle.net/10919/40423.

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The late Mississippian carbonates in the Appalachian Basin, U.S.A., were deposited on a huge, south-facing ramp during long-term Mississippian transgression that formed the Mississippian supersequence. The St. Louis- to Glen Dean interval consists of up to twelve fourth-order depositional sequences (300 to 400 k.y. average duration). The sequences (a few meters to over a hundred meters thick) consist of eolianites, lagoonal carbonate muds, ooid shoals, and skeletal banks, and open marine skeletal wackestone and basinal marion the ramp-slope and basin margin. Sequence boundaries are at the top

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46

Morgan, Glenn Douglas School of Biological Earth &amp Environmental Science UNSW. "Sequence stratigraphy and structure of the tertiary limestones in the Gulf of Papua, Papua New Guinea." Awarded by:University of New South Wales. School of Biological, Earth and Environmental Science, 2005. http://handle.unsw.edu.au/1959.4/22913.

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A sequence stratigraphic study was conducted on the Mendi and Darai Limestone Megasequences in the foreland area of the Papuan Basin in Papuan New Guinea. It involved the integrated use of seismic, wireline log, well core and cuttings, strontium isotope age and biostratigraphic data. This study enhanced the understanding of the structure, stratigraphy and depositional architecture of the limestones, and the morphology of the basin at the time of deposition. The results of the study were integrated with published geological and tectonic models for the Papuan Basin to develop a consistent and

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47

Richardson, Jeffery G. "Miospore Biostratigraphy, Sequence Stratigraphy, and Glacio-Eustatic Response of the Borden Delta (Osagean; Tournaisian/Visean) of Kentucky and Indiana, U.S.A." The Ohio State University, 2003. http://rave.ohiolink.edu/etdc/view?acc_num=osu1048176261.

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48

Ritter, Geoffrey William. "Lithofaces and Sequence Architecture of the Upper Paradox Formation (Middle Pennsylvanian)in the Subsurface Northern Blanding Subbasin, Paradox Basin, Utah." BYU ScholarsArchive, 2018. https://scholarsarchive.byu.edu/etd/7319.

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THE PARADOX Basin is a northwest-southeast trending intracratonic basin that formedin southwestern Colorado, southeastern Utah and adjacent parts of Arizona and New Mexicoduring the late Paleozoic Era. During rise of the adjacent Uncompahgre Uplift (Ancestral RockyMountains) the rapidly subsiding basin was filled with over 2000 m of Permo-Pennsylvaniansediments. Stacked depositional sequences accumulated in three roughly parallel facies belts: anortheastern clastic belt (adjacent to uplift), a central salt and black shale belt, and asouthwestern carbonate belt. Over 400 million barrels of oil

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Dilliard, Kelly Ann. "Sequence stratigraphy and chemostratigraphy of the Lower Cambrian Sekwi Formation, Northwest Territories, Canada." Online access for everyone, 2006. http://www.dissertations.wsu.edu/Dissertations/Spring2006/K%5FDilliard%5F042406.pdf.

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McCrimmon, G. Glen. "Sedimentology and sequence stratigraphy of the lower Cretaceous Clearwater Formation, Cold Lake, Alberta." Thesis, University of Ottawa (Canada), 1996. http://hdl.handle.net/10393/9765.

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Abstract:

The lower Cretaceous (Aptian to Albian) CLearwater Formation at Cold Lake, Alberta contains a complex assemblage of silicicastic strata. On the basis of detailed core analyses, Clearwater Formation strata have been subdivided into eight lithofacies and six recurring, facies associations. These facies associations are: (1) Tidal bar, (2) Sand flat, (3) Tidal-fluvial channel, (4) Fluvial channel, (5) Shoreface to foreshore, and (6) Offshore. Correlation of the facies associations and their bounding time-significant surfaces has led to the interpretation that Clearwater Formation strata are marin

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