Polyphase deformation of possible Proterozoic to Lower Cambrian Miogeoclinal rocks of the Dinkey Creek pendant, central Sierra Nevada
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Authors
Merritt, Nancy J.
Issue Date
1991
Type
Thesis
Language
en_US
Keywords
geology , Dinkey Creek pendant , Sierra Nevada , California , polyphase deformation , structural geology , lithology , folds , foliation , faults , ductile deformation , tectonics , Mackay Science Project
Alternative Title
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.
Citation
Publisher
University of Nevada, Reno
License
In Copyright(All Rights Reserved)