University of Nevada, Reno
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Magmatic interaction in the Crystal Range suite, northern Sierra Nevada batholith, California
Mackay578_Sabine.pdf (20.23Mb)
Mackay578_Sabine_map_0001.jpg (1.368Mb)
Date
1992Type
DissertationDepartment
Geological Sciences and Engineering
Degree Level
Doctorate Degree
Degree Name
Geology
Abstract
The approximately 225-km2 Desolation study area lies at the northern end of the Sierra Nevada batholith, southwest of Lake Tahoe. The area is underlain by early- to middle-Jurassic metasedimentary and metavolcanic rocks of the Mount Tallac pendant, a group of middle-Jurassic plutonic rocks, and several Cretaceous plutons. Extensive glaciated exposures and a diversity of igneous lithologies ranging from leucogranite to anorthosite ideally suit the area for geologic and remote sensing studies.
Description
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Permanent link
http://hdl.handle.net/11714/1658Additional Information
| Committee Member | Exline, Christopher H.; Hibbard, M. J.; Ritter, Dale; Schweickert, Richard A. |
|---|---|
| Rights | In Copyright |
| Rights Holder | Author(s) |