Petrology and structure of the little willow series, Wasatch Mountains, Utah

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Title Petrology and structure of the little willow series, Wasatch Mountains, Utah
Publication Type thesis
School or College College of Mines & Earth Sciences
Department Geology & Geophysics
Author Neff, Thomas Rodney
Date 1962-11
Description The Little Willow area is located on the Wasatch Front between Bells Canyon and Little Willow Canyon. The Little Willow Series is a Middle (?) Precambrian metamorphic complex consisting of mica schist, quartzo-feldspathic schist , banded gneiss meta-conglomerate, quartzite and amphibolite produced from fluvial shales,quartzo- feldspathic sandstones, conglomerates and impure dolomites or basic dikes by dynamo-thermal metamorphism of the epidote-amphibolite fades. The Little Willow foliation generally strikes N-E and steeplydips N-W.
Type Text
Publisher University of Utah
Subject Petrology -- Utah -- Wasatch Mountains; Thesis and dissertation georeferencing project
Dissertation Institution University of Utah
Dissertation Name MS
Language eng
Relation is Version of Digital reproduction of "Petrology and structure of the little willow series, Wasatch Mountains, Utah," J. Willard Marriott Library Special Collections, QE 3.5 1962 N44
Rights Management In the public domain use of this file is allowed in accordance with the Creative Commons Attribution-Noncommercial-No Derivative Works 3.0 United States License, http://creativecommons.org/licenses/by-nc-nd/3.0/us
Format application/pdf
Format Medium application/pdf
Format Extent 31,579,743 bytes
Identifier us-etd2,193571
Source Original: University of Utah J. Willard Marriott Library Special Collections
Conversion Specifications Original scanned on Epson GT-30000 as 400 dpi to pdf using ABBYY FineReader 9.0 Professional Edition.
ARK ark:/87278/s68g91b4
Setname ir_etd
ID 193621
Reference URL https://collections.lib.utah.edu/ark:/87278/s68g91b4
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