2 edition of Sulfide inclusions within the B chromitite, Stillwater Complex, Montana found in the catalog.
Sulfide inclusions within the B chromitite, Stillwater Complex, Montana
M. P. Foose
Bibliography: p. 19-22.
|Statement||by Michael P. Foose and Suzanne W. Nicholson.|
|Series||U.S. Geological Survey bulletin ;, 1674-D|
|Contributions||Nicholson, Suzanne W.|
|LC Classifications||QE75 .B9 no. 1674-D, QE389.2 .B9 no. 1674-D|
|The Physical Object|
|Pagination||iv, 22 p. :|
|Number of Pages||22|
|LC Control Number||88600205|
stillwater complex montana Download stillwater complex montana or read online books in PDF, EPUB, Tuebl, and Mobi Format. Click Download or Read Online button to get stillwater complex montana book now. This site is like a library, Use search box in the widget to get ebook that you want. The stillwater Complex in south-central Montana is a late Archean layered, ultramafic to mafic intrusion emplaced into middle to late Archean metagraywacke, metashale, and iron-formation. Sulfide minerals are concentrated near the base of the intrusion in some chromitite layers, podiform pegmatoids, discontinuous discordant pods or pipes, and numerous thin, stratiform layers.
The Stillwater igneous complex is a large layered mafic intrusion (LMI) located in southern Montana in Stillwater, Sweet Grass and Park complex is exposed across 30 miles (48 km) of the north flank of the Beartooth Mountain complex has extensive reserves of chromium ore and has a history of being mined for chromium. More recent mining activity has produced palladium and. Stillwater Complex, Montana, USA: An igneous complex rich in Chromium and Platinum-group metals.
The Stillwater Complex of Montana is a large layered proper, these sills are closely associated with the Complex mafic intrusion, which has lost its upper part to erosion. in space (Page, ; Zientek, ) and time (Premo et. The Stillwater Complex is a large fragment of a once-enormous ~ Ma ultramafic–mafic layered intrusion. It is exposed on the north flank of the Beartooth Mountains in Montana, a large Laramide uplift. Stillwater layering is complex, in contrast to the comparatively simple layering of the Skaergaard Intrusion in Greenland.
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Sulfide inclusions within the B chromitite of the Stillwater Complex, Montana, provide evidence for complex high-temperature magmatic processes associated with chromiteCited by: 2. Sulfide Inclusions Within the B Chromitite, Stillwater Complex, Sulfide inclusions within the B chromitite Usgs Bulletin D [M.
Foose, Suzanne W. Nicholson] on *FREE* shipping on qualifying offers. The United States Geological Survey (USGS) is a scientific organization created inand is part of the U.S.
government. Their scientists explore our environment and ecosystemsAuthors: M. Foose, Suzanne W. Nicholson. Sulfide inclusions within the B chromitite, Stillwater Complex, Montana [M.
Nicholson, Suzanne W. Foose] on *FREE* shipping on qualifying : Foose, M. Nicholson, Suzanne W. Sulfide inclusions within the B chromitite, Stillwater Complex, Montana Bulletin D By: M.P.
Foose and Suzanne W. Nicholson. Sulfide inclusion within the B chromite of the Stillwater Complex, Montana, provide evidence for complex high-temperature magmatic process associated with chromite precipitation. Stanford Libraries' official online search tool for books, media, journals, databases, government documents and more.
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Sulfide inclusions within the B chromitite low prices and free delivery on eligible : M. Foose, Suzanne W. Nicholson. Sulfide Minerals in the G and H Chromitite Zones of the Stillwater Complex, Montana By NORMAN J PAGE GEOLOGICAL SURVEY PROFESSIONAL PAPER The relationship of the amount, relative abundance, and size of grains of selected sulfide minerals to the crystallization of a basaltic magmaCited by: 9.
Sulfide inclusions within the B chromitite, Stillwater Complex, Montana (DLC) (OCoLC) Material Type: Document, Government publication, National government publication, Internet resource: Document Type: Internet Resource, Computer File: All Authors / Contributors: M P Foose; Suzanne W Nicholson; Geological Survey (U.S.).
Foose MP, Nicholson SW () Sulfide inclusions within the B chromitite, Stillwater Complex, Montana. U.S. Geol. Survey Bull. D, 22 pp Google Scholar Fortin MA, Riddle J, Desjardins-Langlais Y, Baker DR () The effect of water on the sulfur concentration at sulfide saturation (SCSS) in natural by: 5.
Postcumulus amphibole and phlogopite from an olivine cumulate of cyclic unit 2 in the Archean Stillwater Complex, Montanta, containing the B-chromitite, were analyzed with an electron microprobe. Pt-Fe alloy (Pt3Fe) in the J-M Reef of the Stillwater Complex, as exposed in the Stillwater mine, in Montana, occurs intergrown with secondary Fe-Ni-Cu sulfide; together, they replace a Pt-Pd.
Abstract. The Stillwater Complex, Montana, is a layered mafic intrusion containing resources of chromite, platinum, copper, and nickel.
The exploration program for copper and nickel sulfides within the Mountain View area of this igneous body included a series of diamond drillholes located on a : W. Bawiec, J. Schuenemeyer, L. Drew. The geology of the Ga Stillwater Complex in South-Central Montana is reviewed with a focus on the role of volatiles in locally modifying both the crystallization sequence of the evolving parent magma and the initially precipitated solid assemblages to favour olivine ± by: Sulfide Inclusions within the B Chromitite, Stillwater Complex, Montana (United States Geological Survey Bulletin D).
Foose, Michael P. and Suzanne W. Nicholson. Published by United States Government Printing Office. Earth and Planetary Science Letters, 93 () Elsevier Science Publishers B.V., Amsterdam - Printed in The Netherlands Re-Os isotopic investigation of the Stillwater Complex, Montana C.E.
Martin Department of Geology and Geophysics, Yale University, P.O. BoxNew Haven, CT (U.S.A.) Received Janu ; revised version received Ap Cited by: Previous sulfur isotope studies of the Stillwater Complex, and in particular the J-M Reef, have noted the generally restricted range of δ 34 S values in the range of 0 ± ‰ (e.g., Zientek and Ripley, ; Ripley et al., ).
Detailed studies of high-S zones in both the hanging wall of the Reef Package, which contains the J-M Reef, and the footwall within the Reef Package but below the Author: B.W. Wernette, E.M. Ripley, C. Li, R.P. Wintsch. The shape and composition of the PGM within the chromite grains in the Stillwater chromitite layers is not uniform.
Upper and lower layers contain laurites with rounded shapes and an Os content of 7–8%. In the sulfide inclusion-poor middle G layer, the laurites have 5% Os and a predominantly euhedral by: 6. Audio Books & Poetry Community Audio Computers, Technology and Science Music, Arts & Culture News & Public Affairs Non-English Audio Spirituality & Religion.
Librivox Free Audiobook. ROSSO - Ardente How To Fix The Music Business Franko’s Podcast Savior Realty Expert Interviews Roxbury Presbyterian Church Proper Jones Neues von der Aa b s t r a c t Nineteen chromite crystals from the A, B, E, G, H, J and K chromitite layers of the Peridotite Zone of the Stillwater Complex (Montana, USA) have been studied by means of X-ray single crystal diffraction and microprobe by: Fluid and Halide Melt Inclusions of Magmatic Series, Stillwater Complex, Montana, USA J.
J. HANLEY 1*,L2,3,R2 2 1DEPARTMENT OF GEOLOGY, SAINT MARY’S UNIVERSITY, ROBIE STREET, volatiles and grain boundary-hosted sulfide minerals below the J-M reef at near-solidus temperatures, and the post.