Digital Commons Network^™

Structural Geology Of Cutler Dam Quadrangle And Northern Part Of Honeyville Quadrangle, Utah, Douglas A. Sprinkel

All Graduate Theses and Dissertations, Spring 1920 to Summer 2023

The mapped area is located in the north-central part of Utah. The northern part of the mapped area is located in the Basin and Range province and the southern part of the mapped area is located in the Middle Rocky Mountain province. The north-south and east-west dimensions of the mapped area are 11.1 miles and 5.1 miles, respectively.

Paleozoic rocks are exposed in Bear River Narrows, in Cache Butte Divide, and in the Wellsville Mountains. Paleozoic strata, in Bear River Narrows, dip west. The Ordovician Swan Peak Formation crops out in the eastern part of Bear River Narrows. It is …

Dikes Of The Clear Creek Area, Wasatch Plateau, Utah, William Dennis Thomas

All Graduate Theses and Dissertations, Spring 1920 to Summer 2023

The area, covered by this report, includes about 108 square miles in the northeastern part of the Wasatch Plateau in central Utah. Clear Creek, Utah, is near the center of the area.

Stratigraphy of the area is characterized by 18,000 to 20,000 feet of sedimentary rocks above the Precambrian basement. The oldest exposed stratigraphic unit is the 11ancos Formation of late Cretaceous age; the youngest exposed stratigraphic unit is the North Horn Formation of Cretaceous-Tertiary age. The sedimentary rocks are mainly sandstone, shale, and coal. Sandstone and shale are the most abundant.

Structure of the area is characterized by folds …

Geology And Ore Deposits Of The Johnnie District, Nye County, Nevada, Stanley Wayne Ivosevic

UNLV Theses, Dissertations, Professional Papers, and Capstones

The Johnnie district, in the northwestern Spring Mountains, Nye County, Nevada, may have produced a little under 100,000 troy oz of gold, since the discovery of the district in 1890.

An approximately 13,000-ft-thick (4,000 m) section of east-dipping upper Precambrian through Middle Cambrian miogeosynclinal clastic and carbonate rocks is exposed in the district. The strata are, in order of decreasing age, the Johnnie Formation, Stirling Quartzite, Wood Canyon Formation, Zabriskie Quartzite, and Carrara and Bonanza King Formations. These are overlain by Cenozoic units which include and older unit and a younger unit of fanglomerate, the older containing a megabreccia deposit, …

Sedimentology And Diagenesis Of The Monteagle Limestone (Upper Mississippian) -- A High Energy Oolitic Carbonate Sequence In The Southern Appalachian Mountains., Charley Robertson Handford

LSU Historical Dissertations and Theses

No abstract provided.

Experimental Diagenetic Study Of A Modern Lipid-Rich Sediment., William Earl Harrison

LSU Historical Dissertations and Theses

No abstract provided.

The Silicification Of Eocene Deep-Sea Sediments In The Atlantic Ocean., John Arthur Klasik

LSU Historical Dissertations and Theses

No abstract provided.

Diagenesis And Paleohydrology Of A Rudist Reef Complex (Cretaceous), Bandera County, Texas., Timothy Joseph Petta

LSU Historical Dissertations and Theses

No abstract provided.

Glacial Dispersal Of Rocks And Minerals In The Lac Mistassini - Lac Waconichi Area, Quebec, With Special Reference To The Icon Dispersal Train, Ronald Norman Dilabio

Digitized Theses

No abstract provided.

Stratigraphy, Petrology And Diagenesis Of Beekmantown Carbonate Rocks In Eastern Ontario, Peter Strachan Giles

Digitized Theses

No abstract provided.

Petrology And Structure Of The Glen Quadrangle, Southeastern Adirondacks, Ny, Stewart Smith Farrar

Graduate Dissertations and Theses

An outcrop geologic map of The Glen quadrangle has been produced at a scale of 1:24,000. This quadrangle is composed of a sequence of Precambrian rocks which were deformed and recrystallized under clinopyroxene-garnet granulite facies conditions during late Precambrian time. Metasedimentary rocks include calcic and dolomitic marble, metapelites, and metaquartzites. Rocks of known igneous origin include metagabbros, a metanorthosite-anorthositic metagabbro series, and minor unmetamorphosed diabase intrusives. In addition, there are a variety of mineralogically and texturally subdivided granitic-charnockitic gneisses of unknown origin. These rock sequences are correlated, where possible, with previous work in surrounding areas.

Estimates have been made of …

Structural Styles Of The Southern Boundary Of The Sapphire Tectonic Block Anaconda-Pintlar Wilderness Area Montana, Charles Gilbert Wiswall

Graduate Student Theses, Dissertations, & Professional Papers

No abstract provided.

Mineralogy And Structure Of The Stibnite Hill Mine Thompson Falls Montana, Pedro A. Marin Rivera

Graduate Student Theses, Dissertations, & Professional Papers

No abstract provided.

Early Miocene Mammals From The Lemhi Valley Of Idaho, Ralph Nichols

Graduate Student Theses, Dissertations, & Professional Papers

No abstract provided.

Diffusion Of Sediment In The Lee Of Dune-Like Bedforms. (Volumes I And Ii)., Chinmoy Chakrabarti

LSU Historical Dissertations and Theses

No abstract provided.

Diatoms And Other Siliceous Biogenic Remains From Surficial Bottom Sediments Of The Gulf Of Mexico., John Paul Jendrzejewski

LSU Historical Dissertations and Theses

No abstract provided.

Lower Paleozoic Evolution Of West Newfoundland, Robert Keith Stevens

Digitized Theses

No abstract provided.

Pleistocene Local Glaciation In The Adirondack Mountains, New York, Jesse Leo Craft

Digitized Theses

No abstract provided.

Stratigraphy And Petrology Of The Peridotite-Gabbro Component Of The Western Newfoundland Ophiolites, Luca Riccio

Digitized Theses

No abstract provided.