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Author : Utah Geological and Mineralogical Survey
Publisher : Unknown
Page : 424 pages
File Size : 46,5 Mb
Release : 1964
Category : Geology
ISBN : STANFORD:36105008143070
Author : Anonim
Publisher : Unknown
Page : 194 pages
File Size : 46,9 Mb
Release : 1987
Category : Geology
ISBN : UOM:39015049311239
Author : Utah Geological and Mineralogical Survey
Publisher : Unknown
Page : 56 pages
File Size : 45,5 Mb
Release : 1952
Category : Geology
ISBN : CHI:098130734
Author : Anonim
Publisher : Unknown
Page : 120 pages
File Size : 49,8 Mb
Release : 1962
Category : Groundwater
ISBN : UOM:39015012631191
Author : Anonim
Publisher : Unknown
Page : 308 pages
File Size : 47,7 Mb
Release : 1971
Category : Geology
ISBN : PURD:32754069503179
Author : Lehi F. Hintze,Fitzhugh D. Davis
Publisher : Utah Geological Survey
Page : 324 pages
File Size : 47,9 Mb
Release : 2003
Category : Science
ISBN : 9781557916921
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 : Utah Geological and Mineral Survey
Publisher : Unknown
Page : 366 pages
File Size : 40,9 Mb
Release : 1976
Category : Geology
ISBN : PURD:32754069503526
Author : Geological Survey (U.S.),Utah Geological and Mineral Survey,Edgar Baldwin Heylmun,Robert E. Cohenour
Publisher : Unknown
Page : 724 pages
File Size : 52,7 Mb
Release : 1973
Category : Allosaurus fragilis
ISBN : UIUC:30112026930724
Author : Michael D. Hylland,William R. Lund
Publisher : Unknown
Page : 78 pages
File Size : 45,9 Mb
Release : 2003
Category : Government publications
ISBN : PURD:32754078005562
Author : Keith M. Clem,Karl W. Brown
Publisher : Utah Geological Survey
Page : 173 pages
File Size : 53,7 Mb
Release : 1984
Category : Petroleum
ISBN : 9781557910868
The Paradox Basin is a geologic area in southeastern Utah defined by the location of Pennsylvanian salt deposits. The Basin is bounded by the Uncompahgre Uplift to the east and north, the San Rafael Swell, the Circle Cliffs Uplift and the Monument Upwarp to the west, and the Defiance-Zuni Uplift and the Four Corners Platform to the south. The basin is divided into two principal tectonic subprovinces - the Paradox Fold and Fault belt to the north and the Blanding Basin to the south. The Fold and Fault Belt is an area of dominantly northwest-trending salt-cored anticlinal structures. These structures are rooted in the Precambrian basement and have influenced the stratigraphy (deposition) and structure (tectonics) of the Mississippian, Pennsylvanian, and younger formations deposited across them. The Blanding Basin was also a structural low during Pennsylvanian time. It is primarily an area of carbonate-organic mound (bioherm and bioclastic mound) deposition, which forms the most common type of reservoir for petroleum found in the region. This study includes an individual oil and gas field report and a presentation of the regional structure. Sixty-three individual petroleum fields were identified in the Utah portion of the Paradox Basin, and each are represented by data outlining the nature of the petroleum reservoir, along with its geology, structure, and location. The majority of the fields are located in the Blanding Basin subprovince. The regional structure is represented by a structure map of the Ismay zone of the Paradox Formation (Plate 1), elevation at which first salt is encountered in the Paradox Formation (Plate 2), and an isopach map of the salt bed interval in the Paradox Formation (Plate 3). The Ismay Member was chosen to be a representative oil horizon of the Paradox Basin and illustrates the predominant tectonic structures as well as the subtle petroleum related structures. The isopach map of the salt bed interval determines the evaporite boundary in the Basin and illustrates the fold and fault subprovince and corresponding structures. 162 pages + 4 plates
Author : Hellmut H. Doelling
Publisher : Utah Geological Survey
Page : 260 pages
File Size : 43,9 Mb
Release : 1980
Category : Geology
ISBN : 8210379456XXX
Box Elder County displays a variety of lithologic types in each of the major rock divisions: sedimentary, igneous, and metamorphic, in a typical Basin and Range setting. True to the basic structure most of its mountain ranges generally trend north-south, but the Raft River Range trends east-west. Each mountain range exhibits a variety of structural situations: most stratigraphic units are folded and faulted, and many are intruded by igneous rocks. 251 pages + 3 plates
Author : William R. Lund
Publisher : Utah Geological Survey
Page : 77 pages
File Size : 44,9 Mb
Release : 1990
Category : Engineering geology
ISBN : 9781557910936
Geologic exposures in the Salt Lake City region record a long history of sedimentation and tectonic activity extending back to the Precambrian Era. Today, the city lies above a deep, sediment-filled basin flanked by two uplifted range blocks, the Wasatch Range and the Oquirrh Mountains. The Wasatch Range is the easternmost expression of major Basin and Range extension in north-central Utah and is bounded on the west by the Wasatch fault zone (WFZ), a major zone of active normal faulting. During the late Pleistocene Epoch, the Salt Lake City region was dominated by a succession of inter-basin lakes. Lake Bonneville was the last and probably the largest of these lakes. By 11,000 yr BP, Lake Bonneville had receded to approximately the size of the present Great Salt Lake.
Author : Anonim
Publisher : Unknown
Page : 56 pages
File Size : 40,7 Mb
Release : 1983
Category : Geology
ISBN : RUTGERS:39030041197015
Author : Carl L. Ege
Publisher : Utah Geological Survey
Page : 64 pages
File Size : 54,6 Mb
Release : 2005
Category : Business & Economics
ISBN : 9781557917263
Whether you are a geologist, history buff, or rockhound, this booklet will be a helpful guide to Utah?s mining districts. The booklet is divided up into three parts: the first part provides general information on what a mining district is, how many mining districts are in Utah, types of mineral deposits found at these districts, and landownership issues. The second part includes individual mining-district discussions containing information on location, production, history, geology, mineralogy, and current/future operations. The third part includes a glossary of geologic terms and other useful resources in the appendices, such as a descriptive list of minerals found in the districts, geologic time scale, and a list of mineral resources of the mining districts.
Author : Utah Geological and Mineral Survey
Publisher : Unknown
Page : 62 pages
File Size : 46,8 Mb
Release : 1974
Category : Geology
ISBN : PURD:32754069503518