2 edition of Stratigraphy and structure of the Salmo lead-zinc area found in the catalog.
Stratigraphy and structure of the Salmo lead-zinc area
James T. Fyles
|Statement||by James T. Fyles and C.G. Hewlett.|
|Series||Bulletin (British Columbia. Dept. of Mines) ;, no. 41.|
|Contributions||Hewlett, Cecil George, d. 1957.|
|LC Classifications||TN27 .B72 no. 41|
|The Physical Object|
|Number of Pages||162|
|LC Control Number||gs 60000009|
light other fossils and a consequent reinterpretation of both stratigraphy and structure accompanied by a greater appreciation of the complexity of the geology of the region. Part of this area, the belt known as the Salmo lead-zinc area, was restudied by J. T. Fyles and C. G. Hewlett () ofCited by: 4. A major structure, the San Luis–Tepehuanes fault system, separates the northern and southern regions of Mesa Central. The majority of the mineral deposits found in Mesa Central or in its vicinities, especially epithermal deposits, is located on the traces of the major fault systems described above.
Get Textbooks on Google Play. Rent and save from the world's largest eBookstore. Read, highlight, and take notes, across web, tablet, and phone. The Reeves limestone is to metres thick in the mine area. Lead-zinc mineralization, occurring mainly in dolomite near the base of the Reeves Member, varies from 8 to 30 metres in thickness. The limestone and dolomite varies from a blue-green banded type to a white massive type. The dolomites are typically finer grained than the limestones.
mtpd mill operated mine closed until reopened at mtpd in concentrates produced - 4, mt pb conc., 21, mt zn conc. GEOLOGY OF THE CHIBOUGAMAU AREA, QUEBEC, Consolidated Mining & Smelting Company of Canada Limited, February, , scale 1" = 2 miles, folded map, 66 x 76 cm (26 x 30"), hand colored geologic strata shown in 11 colors, 16 base metal deposits located on map, $
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Get this from a library. Stratigraphy and structure of the Salmo lead-zinc area. [James T Fyles; Cecil George Hewlett]. Palaeontology, stratigraphy, and structure of the Jurassic rocks in Salmo map-area, British Columbia, on *FREE* shipping on qualifying offers.
Palaeontology, stratigraphy, and structure of the Jurassic rocks in Salmo map-area, British ColumbiaManufacturer: Dept. of Mines and Technical Surveys, Canada. The problematic history of the strata-bound Salmo lead-zinc deposits, which occur in highly deformed, low-grade metasediments of the southern Kootenay Arc of British Columbia, has been investigated via structural analyses, fabric studies, and minor element determinations in three of the deposits: Reeves MacDonald, Jersey and H.
mines. Three phases of folding have been distinguished: an Cited by: 1. Stratigraphy & Structure Salmo Lead-Zinc Area - By J.T. Fyles and C.G. Hewlett Assessment Report #14 - Victory Group - by J.A.
Mackenzie Assessment Rep or t #63 - - Deer Group By W.T. Irvine Asseesment Report 1/82 - - A~CO Group By W.W. Moorhouse Assessment Rep or t #83 - Arnco Claims - By W.W. Moorhouse. Stratigraphy and structure of the Kootenay Arc in the Riondel area, southeastern British Columbia.
Trygve HöyCited by: Fyles JT, Hewlett C () Stratigraphy and structure of the Salmo lead-zinc area. BC Ministry of Energy and Mines, Bulletin p Google Scholar Gilg HA, Boni M, Hochleitner R, Struck U () Stable isotope geochemistry of carbonate minerals Cited by: 4.
The Geology of the Upper Mississippi Valley Zinc-lead District, Issue 2 figs., 8 tables.Stratigraphy and geologic structure of northern Illinois with special reference to underground water supplies: The Geology of the Upper Mississippi Valley Zinc-lead District, Issue Höy, T.
(): Stratigraphic and Structural Setting of Stratabound Lead- Zinc Deposits in Southeastern British Columbia; Canadian Institute of Mining and Metallurgy, Bulletin, Vol pages The Michaely area was mapped on a regional basis in the mid’s by Jim Fyles of the BC Geological Survey, and is the subject of Bulletin #41 titled “ Stratigraphy and Structure of the Salmo Lead-Zinc Area” The regional setting is described as being in the southern area of the Kootenay arc.
At the Michaely the strike of. Stratigraphy, structure and mineralisation of the Akjoujt area, Mauritania Article in Journal of African Earth Sciences 38(5) April with 70 Reads How we measure 'reads'. Many of the zinc-lead deposits of NE Washington State are poorly known examples of Mississippi Valley Type (MVT) mineralization.
This study compares inclusion fluids from the Josephine Breccia ores with the later cross-cutting sulfide-bearing quartz veins. The breccia ores are cemented mainly by open space fillings of dolomite, sphalerite, quartz, galena, jasperoid and by: 3.
Geological Map of the Salmo Lead-Zinc Area, Sc. ln:2,' - accomp. Bulletin Jack Pot mine (West Zone), (Geol J.T. and Hewlett, C.G. ; Stratigraphy and Structure of the Salmo Lead-Zinc Area; Bulle pp. British Columbia Dept. of Mines, Mineral Policy Sector and stratigraphic correlation has not been.
The diagnostic feature of tectonic wedging and delamination is a reversal in vergence between the bottom and the top of the wedge. Conspicuous tectonic overprinting (‘polyphase folding’) characteristically occurs above the wedge, and is commonly described as ‘backfolding’ and ascribed to polyphase by: 4 GEOLOGY OF UPPER MISSISSIPPI VALLEY ZINC-LEAD DIST.
PREVIOUS WORK 0 The first geologic mapping of parts of the area included in the Dubuque South quadrangle was done by D. Owen in (Owen, ). The purpose of his work was to evaluate mineral-bearing public lands.
Whitney () and C. White () deCited by: 6. Stratigraphy and structure of the Kootenay Arc in the Riondel area, southeastern British Columbia Article in Canadian Journal of Earth Sciences 14(10) February with 8 Reads. - Stratigraphy and Structures of the Salmo Lead-zinc Area Figure 2: Generalized Structural Map of the Salmo Lead-zinc Area Figure 3 - Sheet A: Geological Map of the Salmo Lead-zinc Area Figure 3 - Sheet B Figure 3 - Sheet C: Porcupine Creek Area.
However, the relationship between MVT ore-forming processes and thrusting is unclear. The km-long Sanjiang Metallogenic Belt in Tibetan Plateau is an important thrust-controlled MVT ore province with Mt at –% Pb, –% Zn.
The Zhaofayong MVT ore cluster in the Changdu area Cited by: card 2 - \ ref. zn 8 ref. n.t.s. area 82 f/3 region du s.n. r.c. product zinc produit province or province ou british territory territoire name of property aspen, bell nom de la propri~t~ history of exploration and development (continued).
contains carbonate-hosted lead-zinc deposits. The Rossland camp (Fyles, ; Höy and Dunne, ) The deposits of the Ymir-Nelson area have produced more t kg of gold andkg of silver primarily from vein deposits in the Stratigraphy and structure of the Salmo lead-zinc area; B.C.
Department of Mines, Bulle Part I: Jurassic to mid-Cretaceous. Canadian Journal of Earth Sciences 20 (12): Link, Fyles, J.T., and Hewlett, C.G. Stratigraphy and structure of the Salmo lead-zinc area. BC Ministry of Energy, Mines and Natural Gas, Bulle p.
Klepacki, D.W. Stratigraphy and structural geology of the Goat Range area Cited by: 3. Stratigraphy and Structure of the Maverick Basin and Devils River Trend, Lower Cretaceous, Southwest Texas: A Field Guide and Related Papers, Pages Stratigraphy of the Lower Cretaceous (Albian) Salmon Peak Formation of the Maverick Basin, South Cited by: 3.Palaeontology, stratigraphy, and structure of the Jurassic rocks in Salmo map-area, British Columbia.
[Ottawa] Dept. of Mines and Technical Surveys, Canada  (OCoLC) Document Type: Book: All Authors / Contributors: Hans Frebold; H W Little.McDonald, J.D.,Structural environment of the Salmo type lead-zinc deposits: State of Washington Department of Natural Resources Bulletin, no.
61, p. 55 Muraro, T.W.,Metamorphism of zinc-lead deposits in southeastern British Columbia, in Tectonic history and mineral deposits of the Western Cordillera: Canadian Institute of Mining and Metallurgy Special Volume, no. 8.