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Polyphase deformation of possible Proterozoic to Lower Cambrian Miogeoclinal rocks of the Dinkey Creek pendant, central Sierra Nevada

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Author
Merritt, Nancy J.
Advisor
Schweickert, Richard A.
Date
1991
Type
Thesis
Department
Geological Sciences and Engineering
Degree Level
Master's Degree
Degree Name
Geology
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Abstract
The structural and stratigraphic re-evaluation of the Dinkey Creek pendant reveals possible Proterozoic to Lower Cambrian miogeoclinal sediments along the axis of the Sierra Nevada batholith. Polyphase deformation has been studied in the area.
Description
Online access for this thesis was created in part with support from the Institute of Museum and Library Services (IMLS) administered by the Nevada State Library, Archives and Public Records through the Library Services and Technology Act (LSTA). To obtain a high quality image or document please contact the DeLaMare Library at https://unr.libanswers.com/ or call: 775-784-6945.
Permanent link
http://hdl.handle.net/11714/1515
Subject
geology
Dinkey Creek pendant
Sierra Nevada
California
polyphase deformation
structural geology
lithology
folds
foliation
faults
ductile deformation
tectonics
Mackay Science Project
 
Additional Information
Committee MemberHibbard M. J.; Exline, Christopher H.
RightsIn Copyright(All Rights Reserved)
Rights HolderAuthor(s)
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