3 edition of Radioactive Quartz-Pebble Conglomerates of the Sierra Madre and Medicine Bow Mountains, Wyoming found in the catalog.
Radioactive Quartz-Pebble Conglomerates of the Sierra Madre and Medicine Bow Mountains, Wyoming
Geological Survey of Wyoming Open File 78-3
|The Physical Object|
|Number of Pages||49|
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Buy Radioactive quartz-pebble conglomerates of the Sierra Madre and Medicine Bow Mountains, southeastern Wyoming: Final report by Robert S Houston (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Robert S Houston.
The rocks in Canada contain major deposits of uranium in quartz-pebble conglomerates near the base of the metasedimentary sequence. Similar conglomerates in the Deep Lake Formation in the Medicine Bow Mountains of southeastern Wyoming are slightly radioactive and may contain deposits of uranium and other valuable heavy metals.
rocks of the Sierra Madre and Medicine Bow Mountains of southeastern Wyoming contain radioactive quartz-pebble conglomerates of possible economic interest. These conglomerates do not contain ore-grade uranium in surface outcrops, but an earlier report on the geochemistry of the Arrastre Lake area of the Medicine Bow Mountains shows thatCited by: 2.
Book: Stratigraphy and uranium potential of early proterozoic metasedimentary rocks in the Medicine Bow Mountains, Wyoming. Author of Radioactive Quartz-Pebble Conglomerates of the Sierra Madre and Medicine Bow Mountains, Wyoming, Mineral Resources of the Wind River Basin and Adjacent Precambrian Uplifts, Exploration for diamond-bearing kimberlite in Colorado and Wyoming, Exploration for Diamondiferous Kimberlite, Gold districts of Wyoming, General Review of Northern Colorado.
OFR 78 - 3 / Glass, G. / RADIOACTIVE QUARTZ-PEBBLE CONGLOMERATES OF THE SIERRA MADRE AND MEDICINE BOW MOUNTAINS, SOUTHEASTERN WYOMING, 4 figs., 2 plates, 4 tables (table 4 is missing), 49 pages, photocopy, used, $ This volume is a geostatistical resource estimate of uranium and thorium in quartz-pebble conglomerates, and is a companion to Volume 1: The Geology and Uranium Potential to Precambrian Conglomerates in the Medicine Bow Mountains and Sierra Madre of Southeastern Wyoming; and to Volume 2: Drill-Hole Data, Drill-Site Geology, and Geochemical Data from.
In Medicine Bow Mountains and Sierra Madre. Libby Creek Group Pelitic schist, amphibole schist, quartzite, diamictite, quartz-pebble conglomerate, and marble. Mowry and Thermopolis Shales (Lower Cretaceous) at surface, covers % of this area.
gjbx / karlstrom, k. / national uranium resource evaluation, volume 2: drill hole data, drill site geology, and geochemical data from the study of precambrian uraniferous conglomerates of the medicine bow mountains and the sierra madre of southeastern wyoming, grand junction,pb, pages, 2 plates (in pocket), 57 figs., 19 tables.
Dan Hausel () Geology and Mineralization of the Cooper Hill Mining District, Medicine Bow Mountains, Southeastern Wyoming. Wyoming Geological Survey Report of Investigation Data: Mineral Data: Click here to view Fuchsite data: Locality Data: Click here to view Quartz pebble conglomerate, Cooper Hill District, Carbon Co., Wyoming, USA.
In both the Sierra Madre and Medicine Bow Mountains the base of the miogeoclinal succession north of the Cheyenne belt is a suite of conglomerates and quartzites, the Deep Lake Group.
The Deep Lake Group is a fining up- PROTEROZOIC MINERAL DEPOSITS NEAR PLATE MARGINS, WYOMING by: 5. New field and structural data show that the Cheyenne belt, as defined in the Medicine Bow Mountains, extends into the eastern Sierra Madre This ductile shear zone is truncated by a Precambnan cataclastlc thrust fault in the central and western Sierra Madre The bend in the trend of the Cheyenne belt appears to be associated with the thrusting Cited by: 9.
Quartz-Pebble-Conglomerate Gold Deposits Mineral Deposit Models for Resource Assessment Scientific Investigations Report P Lake in. Proterozoic age quartz pebble conglomerate occurs in the thick miogeoclinal wedge in the northern Medicine Bow Mountains and Sierra Madre.
These conglomerates were of considerable interest in the late s after they were discovered to be radioactive (Houston and Karlstrom, ). During the mapping of these conglomerates some samples were. Worldwide, platinum-group metals (PGE) show a strong affinity for large, intracontinental, layered, mafic complexes of tholeiitic affinity.
Precambrian uranium-bearing quartz-pebble conglomerates: exploration model and United States resource potential. SciTech Connect. Houston, R.S.; Karlstrom, K.E.
Preliminary report on radioactive conglomerates of Middle Precambrian age in the Sierra Madre and Medicine Bow Mountains of southeastern Wyoming. USGS Publications Warehouse. Hous. Wyoming's Laramie Mountains, or quartz pebble conglomerate from Wyoming's Snowy Range.
A scarcity of sediments between 2 million YBP makes assessment of the early Quaternary speculative. is possible that significant erosion of the Ogallala and overlying younger strata occurred during the Pleistocene. About The Product. Published by the American Geophysical Union as part of the Field Trip Guidebooks Series.
Thursday, J (Snyder): Vehicle caravan proceeds through geology stops in Archean metasedimentary rocks with unusually well-preserved primary structures in Hartville uplift to Bunkhouse Motel, Guernsey, Wyoming ( ). Hausel, W.D.,Reconnaissance notes and assay of banded chert, Sierra Madre range, Carbon County, Wyoming: Geological Survey of Wyoming unpub Mineral Report MR, 3 p.
Hausel, W.D.,Assay report on tenorite-stained samples from the Fletcher Park area, Sierra Madre, Wyoming: Geological Survey of Wyoming unpub Mineral Report MR, 3 p.Uranium mining is the process of extraction of uranium ore from the ground.
(in Canada), phosphate, Precambrian quartz-pebble conglomerate, collapse breccia pipes (see Arizona breccia pipe uranium mineralization) InCongress passed the Uranium Mill Tailings Radiation Control Act (UMTRCA), a measure designed to assist in the.DR.
KARL E. KARLSTROM - BIOGRAPHICAL SKETCH Karl E. Karlstrom is a Professor at the University of New Mexico. His main research interests involve structural geology and tectonics, including evolution of tectonic styles in the Precambrian, processes of continental accretion, assembly, and stabilization, and tectonic evolution of the southwestern U.S.