If you have any problems related to the accessibility of any content (or if you want to request that a specific publication be accessible), please contact (email@example.com)
Polyphase deformation of possible Proterozoic to Lower Cambrian Miogeoclinal rocks of the Dinkey Creek pendant, central Sierra Nevada
AuthorMerritt, Nancy J.
AdvisorSchweickert, Richard A.
Geological Sciences and Engineering
AltmetricsView Usage Statistics
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.
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.