1964
DOI: 10.3133/pp415
|View full text |Cite
|
Sign up to set email alerts
|

Geology and mineral deposits of the Thomas and Dugway Ranges, Juab and Tooele Counties, Utah

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
60
1

Year Published

1975
1975
1992
1992

Publication Types

Select...
5
4

Relationship

0
9

Authors

Journals

citations
Cited by 53 publications
(61 citation statements)
references
References 0 publications
0
60
1
Order By: Relevance
“…Staatz and Carr (1964) first described the tuff, and Lindsey (1979) formally named it for exposures in the Thomas Range. The minimum thickness of the Dell Tuff at Keg Mountain is 150 m. Recent paleomagnetic work by J.L.…”
Section: Dell Tuffmentioning
confidence: 99%
“…Staatz and Carr (1964) first described the tuff, and Lindsey (1979) formally named it for exposures in the Thomas Range. The minimum thickness of the Dell Tuff at Keg Mountain is 150 m. Recent paleomagnetic work by J.L.…”
Section: Dell Tuffmentioning
confidence: 99%
“…The only other occurrence of quartzite in rocks of this approximate age known to us is in the Lamb Dolomite of Middle (? ) and Late Cambrian age of the Dugway Range of western Utah (Staatz and Carr, 1964). The quartzite in the Lamb, however, is probably of early Late Cambrian age.…”
Section: Bloomington Formationmentioning
confidence: 93%
“…The Gibson Jack is assigned to the Lower Cambrian on the basis of its possible correlation with the OleneUus-bearing beds. Lithologic equivalents of the Gibson Jack Formation are not known to be present elsewhere, unless part of the Gibson Jack is the lithogenetic equivalent of the Pioche Shale, as suggested by Maxey (1958, p. 649), and of the Lower Cambrian Cabin Shale and Busby Quartzite of northwestern Utah (Nolan, 1935;Staatz and Carr, 1964).…”
Section: Camelback Mountain Quartzite (Upper Part)mentioning
confidence: 99%
“…We thank Gary Lenz and Ezekiel Rivera for their assistance in preparing minThe igneous rocks of the region can be divided into three groups (termed "assemblages" by Shawe, 1972). They will be described only briefly here, and the reader is referred to Staatz and Carr (1964) and Shawe (1972) for detailed descriptions of their petrography and structural setting.…”
Section: Rate Of Deformation and Earthquakesmentioning
confidence: 99%