Date of Award
1985
Document Type
Thesis
Degree Name
Master of Science (MS)
Department
Ocean & Earth Sciences
Program/Concentration
Geology
Committee Director
Dennis A. Darby
Committee Member
Joseph H. Rule
Committee Member
G. Richard Whittecar
Call Number for Print
Special Collections LD4331.G4T78
Abstract
Fifty three samples were taken from three major rivers and their tributaries in Virginia: the James, Roanoke. and Potomac-Shenandoah Rivers. Samples were obtained from the Valley and Ridge. Blue Ridge and Piedmont provinces. The possible source rock types for these samples were determined by comparison of tributary ilmenite composition with drainage basin rock types. Ilmenite element concentration varied with different rock types. Ti was usually high for the ilmenite derived from non-mafic igneous rocks. Mg and Cr were high for the ilmenite from mafic igneous rocks. Zn was low for metamorphic ilmenite. The ilmenite from sedimentary rocks tended to have a high concentration of Ti and a low concentration of Mn and Zn. Ilmenite composition varied among the three rivers. Discriminant. principal component and cluster analysis were used to analyze these differences.
The sources of southeastern Virginia Pleistocene beach deposits were determined by use of a stepwise discriminant analysis of the ilmenite composition for the beach sand compared to the samples from the three rivers. The oldest sampled beach sand. deposited at the Suffolk Scarp. was probably derived from the ancestral James River. Younger beach sands probably have multiple sources.
Rights
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DOI
10.25777/r8gx-d836
Recommended Citation
Tsang, Yu W..
"The Use of Ilmenite Element Composition for the Determination of Provenance"
(1985). Master of Science (MS), Thesis, Ocean & Earth Sciences, Old Dominion University, DOI: 10.25777/r8gx-d836
https://digitalcommons.odu.edu/oeas_etds/382