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Sunday, November 15, 2020 | History

1 edition of Precambrian deposits of zinc-copper-lead sulfides and zine spinel (gahnite) in Colorado. by D.M. Sheridan and W.H. Raymond. found in the catalog.

Precambrian deposits of zinc-copper-lead sulfides and zine spinel (gahnite) in Colorado. by D.M. Sheridan and W.H. Raymond.

Precambrian deposits of zinc-copper-lead sulfides and zine spinel (gahnite) in Colorado. by D.M. Sheridan and W.H. Raymond.

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Published by U.S. Dept. of the Interior in Washington .
Written in English

    Subjects:
  • Geology, Colorado

  • Edition Notes

    11

    ContributionsRaymond, W.H.
    The Physical Object
    Pagination31 p.
    Number of Pages31
    ID Numbers
    Open LibraryOL22017487M


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Precambrian deposits of zinc-copper-lead sulfides and zine spinel (gahnite) in Colorado. by D.M. Sheridan and W.H. Raymond. Download PDF EPUB FB2

Carbonate-hosted lead-zinc ore deposits are important and highly valuable concentrations of lead and zinc sulfide ores hosted within carbonate (limestone, marl, dolomite) formations and which share a common genetic origin. These ore bodies range from million tonnes of contained ore, to 20 million tonnes or more, and have a grade of between 4% combined lead and zinc to over 14% combined.

Abstract. Zincian spinel or gahnite [(Zn,Fe,Mg)Al 2 O 4] occurs in metamorphosed sulphide-rich rocks, garnet quartzites, quartz-magnetite rocks, aluminous metasediments, barite-magnetite rocks, quartz veins, and pegmatites associated with the Aggeneys base metal deposits, Namaqualand, South n spinel in, sulphide-bearing rocks, is considered to have formed predominantly by Cited by: Studies demonstrate that Pb has been mobilized from Precambrian granitic rocks during epidotization, albitization, and oxidation of iron (brick-red granites) (cf.

DOE, ). These granites can be exceptionally lead rich (DOE et ai., ). No mineral deposits are known to be clearly associated with these possible by: These types of deposits are common worldwide.

Volcanigenic massive sulphi de deposits. Volcanogenic massive sulphide deposits are a major source of copper, zinc, lead, silver and gold. These deposits have been found actively forming at a temperature of degrees Celsius. Zinc is the first element in group 12 of the periodic table; it has an atomic number of 30 and the symbol Zn.

Brass, an alloy of copper and zinc, has been used since the 10th century; today, brass is an important alloy used in home appliances where low friction is required (such as with doorknobs and other fixtures) as well as in the production of musical instruments.

Abstract. The potentiometric titration of water extracts from the upper horizons of taiga-zone soils by salt solutions of heavy metals (Pb, Cu, and Zn) showed that their addition is an additional source of the extract acidity because of the involvement of the metal ions in complexation with water-soluble organic substances (WSOSs).Author: G.

Motuzova, I. Makarychev, M. Petrov. I, pp. i, Published by Elsevier Science Ltd All fights reserved. Printed in Great Britain /98 $+ THE INFLUENCE OF CHALCOPYRITE, GALENA AND PYRITE ON THE SELECTIVE EXTRACTION OF ZINC ]FROM BASE METAL SULPHIDE CONCENTRATES T.J.

HARVEY~ and W.T. YENt GeoBiotics Inc., Breakwater Ave, Hayward, CAby:.