Academic literature on the topic 'Cobalt ores Geology'

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Journal articles on the topic "Cobalt ores Geology"

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Dehaine, Quentin, Laurens T. Tijsseling, Hylke J. Glass, Tuomo Törmänen, and Alan R. Butcher. "Geometallurgy of cobalt ores: A review." Minerals Engineering 160 (January 2021): 106656. http://dx.doi.org/10.1016/j.mineng.2020.106656.

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Colomban, Philippe, Burcu Kırmızı, and Gulsu Simsek Franci. "Cobalt and Associated Impurities in Blue (and Green) Glass, Glaze and Enamel: Relationships between Raw Materials, Processing, Composition, Phases and International Trade." Minerals 11, no. 6 (2021): 633. http://dx.doi.org/10.3390/min11060633.

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Minerals able to colour in blue (and green in combination with yellow pigments) are limited in number and geologically. After presenting a short history of the use of cobalt as a colouring agent of glass, glaze and enamel in the Western/Mediterranean, Islamic and Asian worlds since Antiquity, we will present the different forms (dissolved ions, natural and synthetic crystalline phases/pigments) of cobalt and associated elements regarding primary (transition metals) and secondary geological deposits (transition metals and/or arsenic, bismuth, silver). Attempts to identify the origin of cobalt h
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Crundwell, F. K., N. B. du Preez, and B. D. H. Knights. "Production of cobalt from copper-cobalt ores on the African Copperbelt – An overview." Minerals Engineering 156 (September 2020): 106450. http://dx.doi.org/10.1016/j.mineng.2020.106450.

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Novakov, Roman, Valentina Kungurova, and Svetlana Moskaleva. "Formation conditions of noble metal mineralization in sulfide cobalt-copper-nickel ores of Kamchatka (on the example of Annabergitovaya Schel ore occurrence)." Journal of Mining Institute 248 (May 25, 2021): 209–22. http://dx.doi.org/10.31897/pmi.2021.2.5.

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The authors present research results, the purpose of which is to study the specifics of noble metal mineralization and its genesis in sulfide cobalt-copper-nickel ores of the Kamchatka nickel-bearing province. The paper is dedicated to one of its many ore occurrences called Annabergitovaya Schel (Annabergite Gap). The material composition of platinoid, silver, gold, bismuth and tellurium minerals, as well as sulfarsenides in the ores of this occurrence was investigated. Based on the data of mineral formation sequence and the use of geosensors, conclusions were drawn regarding the genesis of no
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Meng, Zhiqiang, Yingjun Chu, Zijian Zhang, and Xiaolong Tian. "Comprehensive development and associated cobalt from Hanxing iron ore tailings." World Journal of Engineering 10, no. 6 (2013): 551–56. http://dx.doi.org/10.1260/1708-5284.10.6.551.

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Cobalt is an extremely useful element, but there are very few separate cobalt deposits in China and imported cobalt ores are usually toxic. In order to develop more low-toxicity cobalt resources, China has to encourage exploration and development of this element. Samples are taken from Hanxing iron ore tailings and analyzed by ICP-MS and barium chloride titration experiments. The results indicate that the cobalt content is relatively high in Hanxing iron ore tailings, and some exceed the industrial grade. Therefore, with the depletion of cobalt resources, iron ore tailings are bound to become
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Lebedev, V. I., A. A. Borovikov, L. V. Gushchina, and I. S. Shabalin. "Physico-chemical modeling of hidrothermal mineralization processes at Ni-Co-As (± U-Ag), Co-S-As (± Au-W), Cu-Co-As (± Sb-Ag) deposits." Геология рудных месторождений 61, no. 3 (2019): 31–63. http://dx.doi.org/10.31857/s0016-777061331-63.

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A generalization of the results of the study of the composition of metal-bearing fluids of cobalt deposits of hydrothermal Genesis, formed in different geodynamic settings in connection with the formation of alkaline and alkaline-basite intrusions and dikes. To determine the physical and chemical parameters of ore deposition from fluid inclusions in minerals, both traditional and new instrumental methods of thermobarogeochemistry were used: thermo-and cryometry, RAMAN spectroscopy, concentration of ore and petrogenic elements in individual fluid inclusions were evaluated by LA-ICP-MS. The obta
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Krutov, G. A., N. P. Mikhaylov, B. V. Obraztsov, and R. A. Vinogradova. "NEW DATA AND HYPOTHESES ON THE ORIGIN OF THE COBALT ARSENIDE ORES OF THE BOU AZZER AREA, MOROCCO." International Geology Review 31, no. 3 (1989): 306–16. http://dx.doi.org/10.1080/00206818909465883.

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Trukhin, Yu P., A. A. Balykov, and M. B. Vainstein. "BACTERIAL-CHEMICAL LEACHING OF COBALT-COPPER-NICKEL ORES AND THE TECHNOLOGICAL SCHEME OF PROCESSING OF PRODUCTIVE SOLUTIONS OF NICKEL AND COBALT." Mining informational and analytical bulletin, S35 (2017): 5–22. http://dx.doi.org/10.25018/0236-1493-2017-12-35-5-22.

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Ntakamutshi, Patrick Tshibanda, Méschac-Bill Kime, Mutamba Edouard Mwema, Banka Richard Ngenda, and Tshamala Arthur Kaniki. "Agitation and column leaching studies of oxidised copper-cobalt ores under reducing conditions." Minerals Engineering 111 (September 2017): 47–54. http://dx.doi.org/10.1016/j.mineng.2017.06.001.

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Dehaine, Quentin, Lev O. Filippov, Inna V. Filippova, Laurens T. Tijsseling, and Hylke J. Glass. "Novel approach for processing complex carbonate-rich copper-cobalt mixed ores via reverse flotation." Minerals Engineering 161 (January 2021): 106710. http://dx.doi.org/10.1016/j.mineng.2020.106710.

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Dissertations / Theses on the topic "Cobalt ores Geology"

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Fay, Hannah Isabel. "Studies of Copper-Cobalt Mineralization at Tenke-Fungurume, Central African Copperbelt; and Developments in Geology between 1550 and 1750 A.D." Diss., The University of Arizona, 2014. http://hdl.handle.net/10150/319897.

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The contents of this dissertation fall into two broad areas: geology and history of geology. Although apparently unrelated, the two categories in fact parallel one another. The development of geological systems finds a mirror, on a shorter timescale, in the development of the human understanding of geological systems. The present state of a science - like the present state of an earth system - represents the concatenation of many subtle or evident processes and influences operating over time. Moreover, the events of the past condition the state of the present in science as well as in objects o
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Llorca, Sylvie. "Les concentrations cobaltiferes supergenes en nouvelle-caledonie : geologie, mineralogie." Toulouse 3, 1986. http://www.theses.fr/1986TOU30231.

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La repartition dans les profils des concentrations cobaltiferes est controlee par deux mecanismes qui interferent: le premier consiste en une accumulation progressive du cobalt dans une tranche donnee de profil correspondant au toit des alterites silicatees, au fur et a mesure de l'approfondissement de l'alteration; le second consiste en une migration progressive du cobalt depuis les zones hautes vers les depressions du toit silicate, formees par la roche en cours d'alteration. Le cobalt est porte par des produits noirs caracteristiques des divers milieux de depot
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Books on the topic "Cobalt ores Geology"

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Nash, J. Thomas. Geology and geochemistry of synsedimentary cobaltiferous-pyrite deposits, Iron Creek, Lemhi County, Idaho. U.S. G.P.O., 1989.

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Book chapters on the topic "Cobalt ores Geology"

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Wothers, Peter. "Goblins and Demons." In Antimony, Gold, and Jupiter's Wolf. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780199652723.003.0008.

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The belief that there were no more than seven metals persisted for hundreds of years, and it was not until the seventeenth century that the inconvenient, inescapable realization came that there were probably many more. I’ve already mentioned Barba’s report from 1640 about the new metal bismuth; it was one of a number of metals or metal-like species that began to be noticed in the sixteenth and seventeenth centuries. In his History of Metals from 1671, Webster begins Chapter 27: ‘Having now ended our Collections and Discourse of the seven Metals, vulgarly accounted so; we now come to some others, that many do also repute for Metals; and if they be not so, at least they are semi-Metals, and some of them accounted new Metals or Minerals, of that sort that were not known to the Ancients.’ In the chapter Webster speaks of antimony, arsenic, bismuth, cobalt, and zinc. While we now understand these as distinct elements, earlier on there was great confusion, with the names being used for compounds rather than the elements themselves—and, furthermore, the different compounds and elements often being mistaken for each other. This makes unravelling their history all the more complicated. We’ll start with Barba’s ‘Mettal between Tin and Lead, and yet distinct from them both’: bismuth. The first mention of bismuth predates Barba’s reference by more than one hundred years. The name appears in its variant spelling, ‘wissmad’, in what is probably the very first book on mining geology. This was published around the turn of the sixteenth century and attributed to one Ulrich Rülein von Calw, the son of a miller who entered the University of Leipzig in 1485. Ulrich mentions in passing that bismuth ore can be an aid to finding silver, since the latter is often found beneath it. Consequently, miners called bismuth ‘the roof of silver’. As Webster later put it in his History of Metals, ‘The ore from whence it is drawn . . . is also more black, and of a leaden colour, which sometimes containeth Silver in it, from whence in the places where it is digged up, they gather that Silver is underneath, and the Miners call it the Cooping, or Covering of Silver.’
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