| Publication Type |
thesis |
| School or College |
College of Mines & Earth Sciences |
| Department |
Geology & Geophysics |
| Author |
Neff, Thomas Rodney |
| Title |
Petrology and structure of the little willow series, Wasatch Mountains, Utah |
| 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 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 |
