Current directions in the Diamond Peak Formation, an Upper Mississippian-Lower Pennsylvanian clastic wedge, east-central Nevada
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Authors
Blomquist, John T.
Issue Date
1971
Type
Thesis
Language
en_US
Keywords
geology , Diamond Peak , clastic wedge , cross-laminations , lithology , conglomerates , sandstone , shale , siltstone , lithofacies , cross-bedding , channeling , bedding surfaces , Buck Mountain , ripple marks , Mackay Science Project
Alternative Title
Abstract
In east-central Nevada the Diamond Peak Formation is best described as a clastic wedge, lying to the east of and paralleling the north-northeast/south-southwest tectonic strike of the Antler orogenic belt.
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