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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
1

LATE ORDOVICIAN SEISMITES OF KENTUCKY AND OHIO: A SEDIMENTOLOGICAL AND SEQUENCE STRATIGRAPHIC APPROACH

MCLAUGHLIN, PATRICK IAN 27 September 2002 (has links)
No description available.
2

A Phylogenetic and Paleobiogeographic Analysis of the Ordovician Brachiopod <i>Eochonetes</i>

Bauer, Jennifer E. 09 June 2014 (has links)
No description available.
3

Faunal Distribution Across the Ordovician-Silurian Boundary in Ohio and Ontario

Fuentes, Stephanie Renee 07 July 2003 (has links)
No description available.
4

Sequence Stratigraphy of the Late Ordovician (Katian), Maysvillian Stage of the Cincinnati Arch, Indiana, Kentucky, and Ohio, U.S.A

Schramm, Thomas J. January 2011 (has links)
No description available.
5

The Ordovician: a window toward understanding abundance and migration patterns of biogenic chert and implications for paleoclimate

Tomescu, Iulia January 2004 (has links)
No description available.
6

The Impact of the Richmondian Invasion on Paleobiogeographic Distribution of Taxa in the Late Ordovician C4 Sequence (Richmondian Stage, Cincinnati, Ohio) Including a Comparison of Range Reconstruction Methods

Dudei, Nicole L. 21 September 2009 (has links)
No description available.
7

Stratigraphic Architecture and Paleogeography of the Juniata Formation, Central Appalachians

Blue, Christina R. 06 May 2011 (has links)
Late 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) "proto-vertisols", (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 (A–D), which are interpreted to be deposited from the inner shelf to the upper shoreface. Isopach and paleocurrent data suggest the shoreline was oriented NE–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 Ordovician–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. / Master of Science
8

Paleobiogeographic Analyses of Late Ordovician Faunal Migrations: Assessing Regional and Continental Pathways and Mechanisms

Lam, Adriane R. 25 August 2015 (has links)
No description available.
9

Attempting to Recreate the Late Ordovician Glaciation with the University of Victoria Earth System Climate Model

Warthen, Seth Tyler 03 November 2016 (has links)
No description available.
10

Analyzing Niche Stability in Late Ordovician Articulated Brachiopod Species during the Richmondian Invasion

Malizia, Richard Walter 26 July 2011 (has links)
No description available.

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