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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
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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.
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