Geochemistry of the Neoproterozoic Johnnie Formation and Stirling Quartzite,
southern Nopah Range, California: Deciphering the Roles of Climate, Tectonics,
and Sedimentary Process in Reconstructing the Early Evolution of a Rifted
Continental Margin
by William A. Schoenborn
BSc. 1978, University of Cincinnati
MSc. 1984, Miami University
A Dissertation submitted to
The Faculty of
The Columbian College of Arts and Sciences
of The e Washington University
in partial fulfillment of the requirements
for the degree of Doctor of Philosophy
January 31, 2010
Dissertation directed by
Christopher M. Fedo
James Carden Associate Professor of Geology
University of Tennessee, Knoxville
UMI Number: 3396960
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UMI 3396960
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The Columbian College of Arts and Sciences of The e Washington University
certifies that William Anthony Schoenborn has passed the Final Examination for the
degree of Doctor of Philosophy as of December 9, 2009. This is the final and approved
form of the dissertation.
Geochemistry of the Neoproterozoic Johnnie Formation and Stirling Quartzite, southern
Nopah Range, California: Deciphering the Roles of Climate, Tectonics, and Sedimentary
Process in Reconstructing the Early Evolution of a Rifted Continental Margin
William A. Sc
Schoenborn, 2010. PhD Geochemistry of the Neoproterozoic Johnnie Formation and Stirling Quartzite, southern Nopah Range, California 来自淘豆网www.taodocs.com转载请标明出处.