Petrogenetic modeling of a potential uranium source rock, Granite Mountains, Wyoming by John S Stuckless

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Published by U.S. Dept. of the Interior, Geological Survey, For sale by the Supt. of Docs., U.S. G.P.O. in [Reston, Va.?], Washington, D.C .

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  • Uranium ores -- Wyoming -- Granite Mountains,
  • Granite -- Wyoming -- Granite Mountains

Edition Notes

Bibliography: p. 16-17

Book details

Statementby John S. Stuckless and A.T. Miesch
SeriesGeological Survey professional paper -- 1225
ContributionsMiesch, A. T., Geological Survey (U.S.)
The Physical Object
Paginationiii, 34 p. :
Number of Pages34
ID Numbers
Open LibraryOL15404229M
LC Control Number80607867

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Get this from a library. Petrogenetic modeling of a potential uranium source rock, Granite Mountains, Wyoming: a study of the origin of a uraniferous granite. [John S Stuckless; A T Miesch; Geological Survey (U.S.),].

Petrogenetic modeling of a potential uranium source rock, Granite Petrogenetic modeling of a potential uranium source rock, Wyoming (DLC) (OCoLC) Material Type: Document, Government publication, National government publication, Internet resource: Document Type: Internet Resource, Computer File: All Authors / Contributors: John S Stuckless; A T Miesch; Geological Survey (U.S.).

MS Book and Mineral Company Geology and Mining History of Wyoming I - Federal Publications R. / RECONNAISSANCE GEOLOGY AND GEOCHRONOLOGY OF THE PRECAMBRIAN OF THE GRANITE MOUNTAINS, WYOMING,pb, 22 pages, 8 figs., 6 tables, $ 8 A.

/ PETROGENETIC MODELING OF A POTENTIAL URANIUM SOURCE ROCK, GRANITE. USGS Professional Papers 5 - Geologic and Mining Related, Numbers - PP / Stuckless, J.

and Miesch, A. / PETROGENETIC MODELING OF A POTENTIAL URANIUM SOURCE ROCK, GRANITE MOUNTAINS, WYOMING,pb, 34 pages, 9 figs., 10 tables, $ 8. USGS Professional Paper Petrogenetic modeling of a potential uranium source rock, Granite Mountains, Wyoming.

Author: Stuckless. 34p. USGS Professional Paper Environmental geology of the Front Range urban corridor and vicinity, Colorado. By Wallace R. Hansen and Eleanor J. Crosby. Pegmatites constitute a category of granite-related ore deposits that are distinct from the magmatic ores disseminated within granites and from hydrothermal assemblages: (1) pegmatites of the rare element class are generated from deeper seated and volatile-undersaturated parental granites that lack disseminated magmatic ores and very rarely.

Phase equilibria modeling has enabled inverse and forward modeling to better characterize the phase relations and chemography of crustal melting for a range of paragneiss and orthogneiss compositions in a chemical system that Petrogenetic modeling of a potential uranium source rock approaches nature (e.g., Johnson et al., ; Brown and Korhonen, ; Korhonen et al., a, ).Cited by: For example, in the Laramie Mountains of southeastern Wyoming, the alkalic Red Mountain and Sybille plutons were intruded into refractory Archean crust and only the most siliceous rocks.

The utilization of radiogenic isotopes and PGE geochemistry offers the potential to evaluate petrologic linkages between various rock suites in a large igneous province and its potential for. Whole rock geochemistry suggests that the Huangshaping granites, especially the granite porphyry, exhibit typical A-type granite characteristics with their enrichment in Si, Rb, U, Th, and Nb and significant depletion in Ba, Sr, Ti, Eu, and P.

Based on the Al, Y and Zr contents as well as the REE patterns of the rocks investigated, the quartz Cited by: You can write a book review and share your experiences.

Other readers will always be interested in your opinion of the books you've read. Whether you've loved the book or not, if you give your honest and detailed thoughts then people will find new books that are right for them. Adequate services, expertise and modern technologies are needed to ensure a sustainable supply of uranium raw materials to fuel both operating and future nuclear power reactors.

Effective regulation, sound environmental management, training and education are required to minimize the impact of uranium mining and production and to contribute to public acceptance of the global. In the reference example a kaolinite- and mica-bearing siliciclastic rock has been taken as host rock and consequently the ternary double-diagram elaborated by Pettijohn et al.

() and Friedman et al. () has been applied most appropriately to describe this clay-bearing rock in more detail. The double-diagram is based on the Cited by:   Field and others to 89 km2 with a median value of 3. deposit had the largest projected area of sulfidebearing rock based on an induced polarization (IP) anomaly (Northern Dynasty Minerals Ltd.

and sulfide-bearing rock projected to the surface (table E1). 1%Mo ppm Au 10 Bing. 8 Yerington Batholith Batu Hijau >%Cu u Cu skarns Limitit of Cu. Cambridge Core - Structural Geology, Tectonics and Geodynamics - The Lithosphere - by Irina ArtemievaCited by: The Ti analogue of lakargiite and Ca analogue of barioperovskite and geikielite; not analogous to tausonite (different structure).

The crystal structure is parent to many important synthetic compounds. The general formula is ABX 3, in which [12] A = larger atoms (cubooctahedral coordination), [6] B = smaller atoms (e.g., Wenk & Bulakh, ).

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Miner. Depos – Åmli, R. (): Secondary uranium and thorium minerals from Einerkilen granite pegmatite in Evje, Southern Norway. Norges Geologiske Undersøkelse [Årbok ]: Lauvland.

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Geology comps from present can be found in bound volumes in the Library under call number Oversize. Chiaradia, M. & Fontboté, L. () Separate lead isotope analyses of leachate and residue rock fractions: implications for metal source tracing in ore deposit studies. Miner.

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90, pp.Google Scholar. Source mantle heterogeneity and its role in the genesis of Late Archean Proterozoic ( - Ga) and Mesozoic ( and Ma Earth Science Reviews.

Proceedings of the International Conferences on Basement Tectonics VOLUME 2 The titles published in this series are listed at the end a/this volume. BASEMENT TECTONICS 8 Characterization and Comparison of Ancient and Mesozoic Continental Margins Proceedings of the Eighth International Conference on Basement Tectonics.

Source rock potential in Pakistan. SciTech Connect. Raza, H.A. Pakistan contains two sedimentary basins: Indus in the. The Stillwater Complex: Integrating Zircon Geochronological and Geochemical Constraints on the Age, Emplacement History and Crystallization of a Large, Open-System Layered Intrusion Corey J Wall Pacific Centre for Isotopic and Geochemical Research, Department of Earth, Ocean & Atmospheric Sciences, University of British Columbia, Cited by: Destruction of the Wyoming craton: seismic evidence and geodynamic processes.

Geology, Vol. 44, 11, pp. United States, Wyoming, Colorado Plateau: Wyoming craton - kimberlites: Abstract: Cratons are old and strong continental cores where the lithosphere is thick and remains largely undeformed for b.y.

Unlike typical cratons, the. 1 Introduction. The Olympic Dam Cu‐U‐Au deposit in South Australia is one of the largest and most valuable ore deposits on Earth, comprising a total resource of billion tonnes grading % Cu, kg/t U 3 O 8, and g/t Au ().Although Olympic Dam is the archetypal member of the iron oxide copper‐gold (IOCG) ore deposit class, an understanding Cited by: Lemmon Rock leucogranite in the Santa Catalina Mountains, Youtcy granite in Redington Pass between the Santa Catalina and Rincon mountains, Espiritu Canyon granite and Wrong Mountain granite in the Rincon Mountains, and Happy Valley granite in the Little (or eastern) Rincon Mountains, as well as theFile Size: 14MB.

Modeling shows that the data are most simply explained by impact events at ca. Ma and ca. Ma, and limits allowable temperatures of heating events between ‐ Ma.

Modeling of solar cycling thermal effects at the lunar surface precludes this. Abrecht, J.,Stability relations in the system CaSiO3-CaMnSi2O6-CaFeSi2O6: Contributions to Mineralogy and Petrology, v. 74, p. Emmermann R () A petrogenetic model for the origin and evolution of the Hercynian granite series of the Schwarzwald.

N Jahrb Mineral Abh – Google Scholar Engel MH, Hare PE () Gas liquid chromatographic separation of amino acids and their derivates. Cr-spinel as a petrogenetic indicator: deducing magma composition from spinels in highly altered basalts from the Japan Sea, Sites and In Tamaki, K., Suyehiro, K., Allan, J.

Whole -rock m ajor -trace element, and radiogenic i sotop ic a nalysis W hole rock t race (e.g., REE) and major element analysis combined with ra diogenic isotope analysis (Nd, Pb) has a long tradition in petrogenetic studies and provide s valuable data for deci phering magmatic process (fractionation, contamination, crustal mixing, depth of.

Full text of "Fifth International Kimberlite Conference: Extended Abstracts" See other formats. The geochronology of layered intrusions, where magma differentiation processes are captured in a wide range of rock textures and structures, represents an essential tool for assessing the evolution of mafic magmatism in the Earth’s by: Anonymous,Discovery of radioactive rock, possibly uranium bearing, has been reported between the South Dakota and Wyoming border, near Belle Fourche, South Dakota, Mining World, v.

15, p. [Periodicals]. Ludwig K R, - Age of Uranium mineralization in the Gas Hills and Crooks Gap Districts, Wyoming, as indicated by U-Pb isotope apparent ages; in Econ. Geol. v74 pp Ludwig K R, Goldhaber MB, Reynolds R L, Simmons K R - Uranium-lead isochron age and preliminary sulfur isotope systematics of the Felder uranium deposit, south.

Geology of Victoria Bibliography Includes index ISBN 1 33 0 1. Geology — Victoria, Australia I. Birch,William D. II. Geological Society of Australia. (Series: Special Publication, Geological Society of Australia; 23). Body text set in Bembo with headings and titles set in Frutiger.

This book is copyright.Mass spectrometry of nanogram-size samples of lead. A. E. Cameron, Dennis Howard. Smith The Bertholène uranium deposit — Mineralogical characteristics and U Pb dating of the primary U mineralization and its subsequent remobilization: Consequences upon the evolution of the U deposits of the Massif Central, France The potential source Cited by: The pyrochlore group gets its name from the generic name pyrochlore which was first introduced by J.

J. Berzelius for a cubic mineral found by N.O. Tank in the s in a syenite pegmatite at Stavern (formerly Fredriksvärn), Norway (Wöhler ).

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