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dc.contributor.authorBlue, Christina Reneeen_US
dc.date.accessioned2014-03-14T20:33:20Z
dc.date.available2014-03-14T20:33:20Z
dc.date.issued2011-03-28en_US
dc.identifier.otheretd-04112011-141942en_US
dc.identifier.urihttp://hdl.handle.net/10919/31683
dc.description.abstractLate Ordovician (Cincinnatian) strata of the central Appalachians provide an opportunity to study the effects of both tectonics and eustasy within a foreland-basin setting. The Juniata Formation consists of red sandstones, siltstones, and shales that were deposited as part of an extensive siliciclastic basin-fill that resulted from the Taconic Orogeny. This study attempts to resolve some of the questions regarding tectonic and eustatic influences on sedimentation by (1) reconstructing the paleogeographic environment of the Juniata Formation and (2) examining the stratigraphic architecture of the Juniata Formation. A combination of both outcrop and subsurface data was analyzed.

Seven facies were identified in this study, including: (1) â proto-vertisolsâ , (2) red shale/mudstone, (3) siltstone/silty mudstone with interbedded sandstones, (4) quartz arenite and sublithic arenite, (5) argillaceous sandstone, (6) hummocky-bedded sandstones and siltstones, and (7) lithic sandstones and conglomerates. These facies are grouped into four facies associations (Aâ D), which are interpreted to be deposited from the inner shelf to the upper shoreface. Isopach and paleocurrent data suggest the shoreline was oriented NEâ SW and detrital sediment was dispersed west and southwest across the basin.

Tectonics controlled the 2nd-Order basin-fill pattern, and these patterns vary along the strike of the basin. Eustatic changes are expressed in two 3rd-Order sequences that were identified in the formation, and possibly in the 4th-Order (?) cycles of Facies Association A. The Ordovicianâ Silurian boundary is expressed as an unconformity throughout the study area, and along-strike variations in the structural setting of the basin were important in its development.

en_US
dc.publisherVirginia Techen_US
dc.relation.haspartBlue_CR_T_2011.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.subjectTuscarora Unconformityen_US
dc.subjectTaconic Orogenyen_US
dc.subjectshoreface depositsen_US
dc.subjectpaleogeographyen_US
dc.subjectLate Ordovicianen_US
dc.subjectJuniata Formationen_US
dc.subjectCentral Appalachian Basinen_US
dc.titleStratigraphic Architecture and Paleogeography of the Juniata Formation, Central Appalachiansen_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.committeechairEriksson, Kenneth A.en_US
dc.contributor.committeememberRead, James Fredricken_US
dc.contributor.committeememberDiecchio, Richard J.en_US
dc.identifier.sourceurlhttp://scholar.lib.vt.edu/theses/available/etd-04112011-141942/en_US
dc.date.sdate2011-04-11en_US
dc.date.rdate2011-05-06
dc.date.adate2011-05-06en_US


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