Published April 1993
by Utah Geological Survey .
Written in English
|The Physical Object|
|Number of Pages||52|
Stratigraphy of the Currant Creek Formation, Wasatch and Duchesne Counties, Utah: Date: Description: The Currant Creek Formation of Late Cretaceous to Early Eocene age is located on the northwestern flank of the Uinta Basin and on the southwestern flank of the Uinta Mountains. A stratigraphic section about 2, feet (~ meters) thick was measured near Crow Creek (east of Cedar City) in order to correlate it to lithostratigraphic units in the Kaiparowits Plateau. The section overlies the Tibbet Canyon Member of the Straight Cliffs Formation (Upper Cretaceous) and underlies the Claron Formation. A summary of Tertiary volcanic stratigraphy of the southwestern high plateaus and adjacent Great Basin, Utah. (Contributions to stratigraphy) (Geological Survey Bulletin B) Babliography: p. Supt. of Docs. no.: I B l. Geology, Stratigraphic-Tertiary. 2. Volcanism-The West. I. Anderson, John Jerome, joint author. by: 4. Stratigraphic Framework of the Cretaceous Mowry Shale, Frontier Formation and Adjacent Units, Southwestern Wyoming Province, Wyoming, Colorado, and Utah By Mark A. Kirschbaum and Laura N.R. Roberts U.S. Geological Survey Digital Data Series DDS–69–D U.S. Department of the Interior U.S. Geological Survey Chapter 15 ofFile Size: 2MB.
central and eastern Utah and western Colorado (Figs. 1, 2, 3). This stratigraphic interval has been documented extensively in the Book Cliffs area in Utah, and its sequence stratigraphy has been interpreted and used as a proxy to trace Cretaceous sea-level variations (Van Wagoner ; Willis ; Willis and Gabel , ; Wood ). These. Stratigraphic correlation using well logs CREWES Research Report — Volume 16 () 1 Well log study and stratigraphic correlation of the Cantuar Formation, southwestern Saskatchewan Shaohua Li, Charles M. Henderson, and Robert R. Stewart ABSTRACT This paper presents the results of a wireline log study on the Cantuar Formation of the. Claron Formation upper member lower member Grapevine Wash Formation Canaan Peak Fm. 35 tectonic breccia (?) Ktm Ksu Kst Kdt Jcw Jcp Jcx Jcc Jtw Jts Jc Kcm Ki Iron Springs Formation a i g h t S t r C l i f f s F m. upper unit Tibbet Canyon Mbr Dakota Fm and Tropic Shale, undivided > 3 2 0 > 1 0 0 2 4 5 0 7 3 5 8 5 0 2 6 File Size: 5MB. Utah Stratigraphic Columns (overview page) These stratigraphic columns are dynamically created (on the fly) from information stored in a database. Information was gathered from a number of sources – see copyright info for more information.
SPATIAL VARIATIONS IN EOLIAN STRATIGRAPHIC ARCHITECTURE OF THE NORPHLET FORMATION, SOUTHWESTERN ALABAMA. A Thesis. by. MARIA ANTONIETA GUTIERREZ AZUAJE. Submitted to the Office of Graduate and Professional Studies of. Texas A&M University. in partial fulfillment of the requirements for the degree of. MASTER OF SCIENCE. Chair of Committee. stratigraphy developed. Teacher note Stratigraphy is usually overlooked in beginning Earth Science classes. However, it is an important tool to the petroleum and mining industries. Stratigraphy is the analysis of different rock formation through time and changing Size: 2MB. Stratigraphic revision of Campanian (Upper Cretaceous) rocks in the Henry Basin, Utah Article (PDF Available) in Mountain Geologist (1) January with Reads How we measure 'reads'. Stratigraphy and Structure of the Beaver Dam Mountains, Southwestern Utah. Lehi F. Hintze. Abstract. The Beaver Dam Mountains in southwesternmost Utah expose a Phanerozoic stratigraphic sequence more than 6 mi thick that rests on a Precambrian complex of gneiss, schist, and pegmatite.