Academic literature on the topic 'Gravure du chrome massif'

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Journal articles on the topic "Gravure du chrome massif"

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SHIRYAEV, Pavel Borisovich, and Nadezhda Vladimirovna VAKHRUSHEVA. "Zonality of ore-forming chrome spinels of medium-chrome and aluminous chromitites of the Voikaro-Syninsky massif." NEWS of the Ural State Mining University, no. 2 (June 15, 2021): 39–47. http://dx.doi.org/10.21440/2307-2091-2021-2-39-47.

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Relevance of the work. The conditions for the formation of chromium ores in alpine-type ultramafites remain a topical subject of research. In recent years, scientific papers have focused on the issue of changing the chemical composition of ore-forming minerals and chromium ores under the influence of deformation and dynamic recrystallization processes accompanying metamorphism. The results of such studies make it possible to formulate a new model of the formation of chromium mineralization taking into account a significant amount of geological data indicating that alpine-type ultramafic rocks
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ALEKSEEV, Aleksandr Valer’evich, and Tat’yana Andreevna SHERENDO. "Composition, structure and magnetic properties of ore chrome spinels of the Klyuchevsky massif (Middle Urals)." NEWS of the Ural State Mining University 1, no. 1 (2020): 73–85. http://dx.doi.org/10.21440/2307-2091-2020-1-73-85.

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The overall objective was to create a geological and geophysical field test site for chromite mineralization and detailed works in order to determine and test the main search criteria for disseminated mineralization. To create a field test site, an area was selected in the southern part of the Klyuchevsky massif characterized by abundant development of disseminated mineralization in the banded dunite-clinopyroxenite complex and strong processes of superimposed metamorphism. This paper gives a piece of research on the composition of chrome spinel from disseminated ores that underwent metamorphi
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Sherendo, Tatyana, Valentin Mitrofanov, Aleksey Vdovin, et al. "Magnetic Clusters in Natural Ferro-Chromian Spinels." Solid State Phenomena 233-234 (July 2015): 587–90. http://dx.doi.org/10.4028/www.scientific.net/ssp.233-234.587.

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The results of investigations of natural iron-chromium spinels of variable composition Fe2+(Cr2-xFex3+)O4 of the chromite-bearing Klyuchevskoi massif (Middle Urals), which are the main carriers of the magnetization of rocks are presented. Substantial changes in the composition and in magnetic structure of accessory chrome-spinels scattered in the host rock are established, unlike the almost unaltered ore-forming chrome-spinels, under the influence of secondary geological processes. To establish the connection between the chrome-spinel changes at the microlevel and features of the geomagnetic f
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Chernyshov, A. I., A. N. Yurichev, and A. V. Kicheeva. "Petrogeochemical characteristics of chrome-bearing ultramafites in the Kurtushibinsky ophiolite belt (Western Sayan)." LITHOSPHERE (Russia) 19, no. 5 (2019): 687–703. http://dx.doi.org/10.24930/1681-9004-2019-19-5-687-703.

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Research subject. The metamorphic ultramafites of the Kalninsky and Ergaksky massifs located in the northeastern part of Western Sayan (Russia) constitute the Kurtushibinsky ophiolite belt. These rocks are considered to be potentially interesting as bearing chromium and noble metals, which fact determines the relevance of this research.Materials and methods. Thin and polished sections of silicate and ore minerals from the ultramafic rocks under study were investigated using a polarizing microscope AxioScop, Carl Zeiss. The chemical composition of minerals was determined by the method of X-ray
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Vakhrusheva, N. V., K. S. Ivanov, V. N. Puchkov, and P. B. Shiryaev. "SUBALKALINE BASALTOIDS IN ULTRAMAFIC ROCKS OF THE RAI-IZ MASSIF (POLAR URALS) AND THEIR PETROGENETIC SIGNIFICANCE." Доклады Российской академии наук. Науки о Земле 509, no. 2 (2023): 208–14. http://dx.doi.org/10.31857/s2686739722602538.

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The composition and age of subalkaline dolerites localized in chromite-bearing ultramafic rocks of the Rai-Iz massif are investigated. Dolerites are traced along tectonic zones inside ultramafic rocks and are not observed beyond their boundaries, spatially tending to deposits and occurrences of chromites.The studied dolerites are characterized by high concentrations of alkalis, TiO2, P2O5, enrichment with large-ion lithophilic elements and Th; the amount of REE varies from 103.3 to 164.2 ppm; (La/Sm)n = 1.3–1.7. The age of subalkaline dolerites was determined by the method 40Ar/39Ar (402.7 ± 3
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Lesnov, F. P., M. Yu Podlipskii, G. V. Polyakov, and S. V. Palesskii. "Geochemistry of accessory chrome-spinellides from rocks of the Ergakskii chrome-bearing hyperbasite massif (western Sayan) and conditions of its formation." Doklady Earth Sciences 423, no. 1 (2008): 1245–49. http://dx.doi.org/10.1134/s1028334x08080138.

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Murzin, V. V., К. N. Malitch, I. Yu Badanina, D. A. Varlamov, and I. S. Chashchukhin. "Mineral assemblages from chromitites of the Alapaevsk dunite-harzburgite massif (Middle Urals)." LITHOSPHERE (Russia) 23, no. 5 (2023): 740–65. http://dx.doi.org/10.24930/1681-9004-2023-23-5-740-765.

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Research subject. Minerals and mineral assemblages of noble elements in chromitites of the Alapaevsk massif. Aim. A systematic mineralogical study of high-chromium (Cr) and alumina-rich (Al) chromitites with the development of a sequence scheme for mineral formation, including platinum-group minerals (PGMs) and gold alloys. Materials and Methods. Samples of high-Cr and Al chromitites from chromite deposits in various parts of the Alapaevsk massif. Scanning electron microscopy (Tescan VEGAII XMU and JSM-6390LV Jeol with EDX INCA Energy 450 X-Max 80 spectrometers) and electron microprobe analysi
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Shiryaev, P. B., Yu V. Erokhin, K. S. Ivanov, V. N. Puchkov, and V. V. Khiller. "About the first discovery of titanium–containing hydroxylclinohumite in podiform chromitite." Доклады Российской академии наук. Науки о Земле 514, no. 1 (2024): 114–21. http://dx.doi.org/10.31857/s2686739724010137.

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For the first time in podiform chromitites, a mineral of the humite group, titanium–containing hydroxylclinohumite, belonging to natural dense water-containing magnesian silicates (DHMS phases), was found. The find was made in chrome ores of the Paity plateau, located in the northern part of the Voikaro-Synyinsky ultramafic massif of the Polar Urals. Chromitites are deposited in the dunite body, which is located at the contact of apoharzburgite amphibole-olivine-antigorite and amphibole-enstatite-olivine metamorphic rocks containing relics of non-serpentinized harzburgites. According to optica
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Ankushev, M. N., V. V. Zaykov, V. A. Kotlyarov, and M. E. Romanenko. "Chrome spinels and accessory mineralization in the weathering crust of the Vladimir deposit, Varshavsky ultramafic massif, southern Urals." Geology of Ore Deposits 58, no. 8 (2016): 697–710. http://dx.doi.org/10.1134/s1075701516080031.

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Bakhterev, V. V. "High-temperature electrical conductivity of chromite ores from the Alapaevsky hyperbasite massif, Middle Urals, as a function of their composition and metamorphism." LITHOSPHERE (Russia) 22, no. 4 (2022): 526–35. http://dx.doi.org/10.24930/1681-9004-2022-22-4-526-535.

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Research subject. Chromite ores and massive chromitites with alumina (low chromium) chrome spinelide (the Podennoye deposit deposit) and chromite ores with high-chromium chrome spinelide (Kurmanovskoye deposit) of the Alapaevsky hyperbasite massif. Materials and methods. Samples of chromite ores and massive chromitites collected during field research were studied in transparent sections using chemical analysis and electrical methods (electrical conductivity, dielectric losses). Results. The temperature dependences of electrical resistance and dielectric losses in the temperature range of 20‒80
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Dissertations / Theses on the topic "Gravure du chrome massif"

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Laourine, Feriel. "Texturation de la surface d’aciers inoxydables par plasmas chlorés et compréhension des mécanismes mis en jeu par l’étude de la gravure du fer, du chrome et du nickel massifs." Electronic Thesis or Diss., Université de Lorraine, 2021. http://www.theses.fr/2021LORR0252.

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La structuration à l’échelle submicronique de la surface des aciers inoxydables permet de leur apporter de nouvelles fonctionnalités, par exemple pour des applications tribologiques et optiques. Cette thèse s’inscrit dans le cadre du projet ANR SPOT qui a pour objectif de structurer à l’échelle submicronique la surface d’aciers austénitiques et martensitiques par gravure sèche. Dans ce travail, nous avons développé un procédé plasma avec un mélange de chlore et d’argon pour la gravure des aciers inoxydables. La mise au point de ce procédé a été réalisée en se basant sur l’étude de la gravure d
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Fandeur, Dik Stefano. "Géochimie et cristallochimie du chrome au cours de l'altération de roches ultrabasiques en Nouvelle-calédonie (Massif du Koniambo)." Paris 7, 2009. http://www.theses.fr/2009PA077035.

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En Nouvelle-Calédonie, 35 Ma d'intense altération et d'érosion de roches ultrabasiques ont permis le développement d'une couverture latéritique riche en éléments traces métalliques (Ni, Cr, Co, Mn). Dans ces sols, ces éléments traces métalliques (ETM) constituent un risque pour l'environnement endémique de la Nouvelle-Calédonie. Parmi ces ETM, le Cr est le plus abondant (jusqu'à 3,8% en poids de Cr₂O₃) mais également le plus toxique, suivant son degré d'oxydation. Après avoir étudié la redistribution des éléments majeurs et traces au cours du développement d'un régolithe de 64 mètres d'épaisse
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Kierczak, Jakub. "Spéciation solide du nickel et du chrome dans un site minier et industriel à usage agricole (Szklary, Pologne)." Limoges, 2007. https://aurore.unilim.fr/theses/nxfile/default/9a2fbfbb-1238-4d3e-af9f-c2d3e533d23f/blobholder:0/2007LIMO4034.pdf.

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Dans le site étudié du Massif de Szklary (Pologne), Ni et Cr sont présents à des concentrations élevées dans deux environnements d’origine distincte : naturelle (sols développés sur serpentinites) et industrielle (haldes de déchets pyrométallurgiques issus de l’exploitation du Ni). L’objectif de cette étude est de localiser les minéraux porteurs d’éléments potentiellement toxiques (EPT), principalement de Ni et Cr, dans ces divers environnements et de comparer leur mobilité dans les conditions actuelles d’altération (climat tempéré transitionnel de Pologne). Ces travaux s’intéressent également
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Al-Khoury, Waël. "Etude structurale par spectrométrie Mössbauer et diffraction des rayons X d'alliage Fe-Cr à l'état massif et en couches minces : transformation de phase autour de la composition équi-atomique." Poitiers, 2006. http://www.theses.fr/2006POIT2303.

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Le but de cette thèse est l'étude structurale des alliages Fe-Cr sous forme massive – transformation de phase ? (cubique centré) ? ? (tétragonal) – et en couche mince, en utilisant principalement la spectrométrie Mössbauer, et en complément, la diffraction des rayons X. Une caractérisation structurale précise de la transformation de phase à 700 °C dans des alliages massifs FeCr à gros grains a été menée. Le résultat le plus pertinent, mis en évidence par l'effet Mössbauer, est l'existence d'une phase intermédiaire appelée ' entre la phase  initiale et la phase  finale. La diffraction des ra
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Book chapters on the topic "Gravure du chrome massif"

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Kislov, Evgeniy V., Vadim S. Kamenetsky, Alexey V. Malyshev, and Vladislav V. Vanteev. "Concentrically-Zoned Mafic-Ultramafic Marinkin Massif, Middle Vitim Highland, Baikal Region, Russia: Inclusions in Chrome Spinel—Key to Mineral Formation Processes." In Springer Proceedings in Earth and Environmental Sciences. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-49468-1_15.

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Conference papers on the topic "Gravure du chrome massif"

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Савицкий, Александр, Вера Ильна, and Владимир Кевлич. "Preliminary assessment of the radiation-hygienic situation at the Aganozero complex deposit." In Mineralogical and technological appraisal of new types of mineral products. Karelian Research Center of RAS, 2019. http://dx.doi.org/10.17076/tm13_13.

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The Aganozero chromium ore deposit, located in the Pudozh District, Karelia, is a complex object for ore and non-metalliferous useful minerals such as chromium ores, platinoids, chrome spinellids as well as Mg-bearing and high-Mg raw materials, e.g. serpentinite, olivinite, dunite and building materials. The primary goal of the present paper is to assess the radiation-hygienic situation at the Burakovian-Shalozero-Aganozero massif, which comprises the Aganozero deposit. Our assessment is essential in connection with the Megaproject to be launched in Karelia, where the Aganozero deposit will pl
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