B031: Cambrian formations of the Eureka and Pioche districts, Nevada PDF Download
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Author: D. M. Lemmon
Publisher: NV Bureau of Mines & Geology
ISBN:
Category :
Languages : en
Pages : 68
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Book Description
Author: D. M. Lemmon
Publisher: NV Bureau of Mines & Geology
ISBN:
Category :
Languages : en
Pages : 68
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Book Description
Author: Lehi F. Hintze
Publisher: Utah Geological Survey
ISBN: 1557916926
Category : Science
Languages : en
Pages : 324
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Book Description
This bulletin serves not only to introduce the non-geologist to the rich geology of Millard County, but also to provide professional geologists with technical information on the stratigraphy, paleontology, and structural geology of the county. Millard County is unique among Utah’s counties in that it contains an exceptionally complete billion-year geologic record. This happened because until about 200 million years ago the area of present-day Millard County lay near sea level and was awash in shallow marine waters on a continental shelf upon which a stack of fossil-bearing strata more than 6 miles (10 km) thick slowly accumulated. This bulletin summarizes what is known about these strata, as well as younger rocks and surficial deposits in the county, and provides references to scientific papers that describe them in greater detail. Mountains North 30 x 60 (1:100,000-scale) quadrangles. These companion maps and this bulletin portray the geology of Millard County more completely and accurately than any previously published work.
Author: Malay Mukul
Publisher: Utah Geological Survey
ISBN: 1557916152
Category : History
Languages : en
Pages : 61
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Book Description
Proterozoic sedimentary rocks in the Sheeprock and the adjacent West Tintic Mountains in northcentral Utah were thought to be deformed and transported along the Sheeprock and Pole Canyon thrusts during the Cretaceous to early Tertiary Sevier Orogeny. Evidence from the observed stratigraphy, stratigraphic separation diagrams, downplunge projections of the structure, large-scale relationships between bedding and cleavage orientations, microstructural observations and finite strain data indicate that the Pole Canyon and the Sheeprock thrusts are the same fault, the Sheeprock thrust. The Sheeprock thrust was folded into a gentle synform and subsequently offset by motion along the Indian Springs fault. Based on the offset pattern of the folded Sheeprock thrust along the Indian Springs fault and multiple slickenlines on the Indian Springs fault, two components of motion are recognized; a dextral strike-slip component and a dip-slip component of motion where the southern block is downthrown. The relative age between the two components is not clear.
Author: Joan Gilbert Martin
Publisher:
ISBN: 9781890625085
Category : Authors, American
Languages : en
Pages : 192
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Book Description
Author: Lewis Gardner Westgate
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 106
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Book Description
Author: Arnold Hague
Publisher: BoD – Books on Demand
ISBN: 3385412501
Category : Fiction
Languages : en
Pages : 438
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Book Description
Reprint of the original, first published in 1892.
Author: Harry Eugene Wheeler
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 52
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Book Description
Author: Lewis Gardner Westgate
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 79
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Book Description
