Academic literature on the topic 'Tin ores'

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Journal articles on the topic "Tin ores"

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Liu, Si Qing, Bao Liang Ge, Bao Xu Song, and Wan Ping Wang. "Some Considerations on Processing Cassiterite-Bearing Polymetallic Sulphide Ores in China." Advanced Materials Research 496 (March 2012): 453–56. http://dx.doi.org/10.4028/www.scientific.net/amr.496.453.

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Tin resources are mainly distributed in Yunnan and Guangxi autonomous regions, China. Tin ores in these areas are characterized by polymetallic constituents, including copper, zinc, lead and other associated elements that can be recovered. Due to the complex mineral composition and texture of the ores, gravity concentration, flotation as well as some combined processing techniques used in some major concentrators are reviewed and discussed. Case study shows that the comprehensive utilization of the tin ores can be realized to produce some marketable products for smelters. But much work on reco
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I., Blinov, and Vinogradov N. "Mineral Composition of Ores Used at Ustye-I, a Fortified Settlement of the Bronze Age (Chelyabinsk Region)." Teoriya i praktika arkheologicheskikh issledovaniy 33, no. 4 (2021): 166–84. http://dx.doi.org/10.14258/tpai(2021)33(4).-10.

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At the fortified settlement of the Bronze Age, Ustye-I (South Trans-Urals), metal products of copper, arsenic and tin bronzes, numerous fragments of metallurgical slags, as well as fragments of copper ores have been discovered. According to the results of early studies, pure copper predominates among metal items (53.4% of finds), but also a significant part contains an admixture of arsenic (25.4% of finds), tin (13.6% of finds) and both components simultaneously (7.6% of finds). Several alloying components of the samples are simultaneously found in slags: Pb (50% of cases), As (49% of cases),
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Бровендер, Ю. М. "To the issue of tin bronzes over the area of the Dnieper-Don region in the late bronze age." ВІСНИК СХІДНОУКРАЇНСЬКОГО НАЦІОНАЛЬНОГО УНІВЕРСИТЕТУ імені Володимира Даля, no. 3(259) (February 18, 2020): 13–17. http://dx.doi.org/10.33216/1998-7927-2020-259-3-13-17.

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The paper is devoted to tin ores as an alloying impurity in the bronze production by the ancient population of the Dnieper-Don region in the Late Bronze Age. The eastern and western supply vectors providing the local population with both ore (cassiterite) and its products are considered. The author draws attention to the assumptions of some researchers not confirmed by geological surveys about the possibility of finding tin deposits in the Donbass and Krivoy Rog basin, which could probably have been developed in the Early Metal Age. An opinion was given regarding the production of bronze from
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Peng, Zhenan, Makoto Watanabe, Kenichi Hoshino, and Yasuhiro Shibata. "Ore mineralogy of tin-polymetallic (Sn-Sb-FePb-Zn-Cu-Ag) ores in the Dachang tin field, Guangxi, China and their implications for the ore genesis." Neues Jahrbuch für Mineralogie - Abhandlungen 175, no. 2 (1999): 125–51. http://dx.doi.org/10.1127/njma/175/1999/125.

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Rodliyah, I., R. Wijayanti, A. Septiarani, A. Sudrajat, and D. Firmansyah. "The extraction of tin (Sn) from primary tin ore deposits using wet chlorination." IOP Conference Series: Earth and Environmental Science 882, no. 1 (2021): 012007. http://dx.doi.org/10.1088/1755-1315/882/1/012007.

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Abstract More than half of the world’s tin production is from secondary ore deposits. However, along with its depletion, PT Timah Tbk has explored and mined the primary deposits in Belitung, one that is expected to become tin’s new source. Tin was found liberated as cassiterite in the secondary deposits, while in the primary, it was associated with other minerals requiring more complex processing. Therefore, a suitable technology is needed to extract the tin from the primary ore deposits. This research aims to observe the extraction of tin from primary deposits (oxide and skarn ores) using HCl
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Pavlova, G. G., S. V. Palessky, A. S. Borisenko, A. G. Vladimirov, Th Seifert, and Luu Anh Phan. "Indium in cassiterite and ores of tin deposits." Ore Geology Reviews 66 (April 2015): 99–113. http://dx.doi.org/10.1016/j.oregeorev.2014.10.009.

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Gaspar, O., and A. Pinto. "The ore textures of the Neves-Corvo volcanogenic massive sulphides and their implications for ore beneficiation." Mineralogical Magazine 55, no. 380 (1991): 417–22. http://dx.doi.org/10.1180/minmag.1991.055.380.11.

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AbstractThe Neves-Corvo mine opened officially in December 1988 and it is already the biggest producer of copper in the Iberian Pyrite Belt (IPB). Tin production started in 1990. The ore deposits of the IPB are related to felsic submarine volcanism which developed during the lower Tournaisian to the middle Visean. At the end of the first phase of Hercynian deformation in the middle Westphalian, the ore deposits were affected by low-pressure metamorphism producing schistosity and prehenite-pumpellyite greenschist facies assemblages in the volcanogenic sediments of the IPB.The unique nature of t
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Grigoriev, S. A. "Development of metallurgy of copper and copper alloys in China in the 2nd millennium BC." VESTNIK ARHEOLOGII, ANTROPOLOGII I ETNOGRAFII, no. 2(57) (June 15, 2022): 31–43. http://dx.doi.org/10.20874/2071-0437-2022-57-2-3.

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The first rare metal finds in China are dated to the Neolithic period, but most of them belong to its final phase. For this period, pure copper is known, very rare arsenic alloys, probably smelted from ore with arsenic admixtures. At the beginning of the 2nd millennium BC, in Gansu, the technology of smelting ore with the following alloying with arsenic, occasionally tin minerals were borrowed from an unknown source. This technology spread to the east, and is present in the Erlitou II layer. At the beginning of the Erlitou III phase (which corresponds to the beginning of the Shang dynasty), th
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Rodliyah, I., R. Wijayanti, K. N. Hidayat, E. A. Dianawati, A. Sudrajat, and D. Firmansyah. "Beneficiation of cassiterite from primary tin ores using gravity and magnetic separation." IOP Conference Series: Earth and Environmental Science 882, no. 1 (2021): 012008. http://dx.doi.org/10.1088/1755-1315/882/1/012008.

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Abstract Alluvial tin ore deposit of PT. Timah is predicted to be depleted in the next 5 to 10 years. Finding a new source of tin ore is important for the company’s sustainability. PT. Timah has been exploring for primary tin ore. Tin (Sn) content in primary tin ore ranges from 0.2 – 1.0%. The Sn particles liberated in the cassiterite mineral are above 50% so they can be processed by the physical separation method. This research aims to observe the beneficiation of cassiterite from primary tin ore (oxide and skarn samples) using gravity and magnetic separation. The cassiterite concentrate prod
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Liu, Si Qing, Xiong Tong, Bao Xu Song, and Wan Ping Wang. "Case Study on Beneficiation of Cassiterite-Polymetallic Sulphide Ores." Advanced Materials Research 511 (April 2012): 28–31. http://dx.doi.org/10.4028/www.scientific.net/amr.511.28.

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Cassiterite-polymetallic sulphide ore contains multi-elements that can be recovered in beneficiation. Case studies on processing two major tin deposits in Gejiu and Dachang regions are reviewed. Results show that the joint process of flotation and gravity separation has proven to be effective in treating the ores for its high efficiency and relatively small environmental impact. Flotation of tin minerals is considered as a supplementary technique for concentrating cassiterite from the slime produced in the joint process. The joint process is still a promising process in treating the cassiterit
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Dissertations / Theses on the topic "Tin ores"

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Saad, Allan Emile. "A petrological study of the tin-tungsten deposit at Renosterkop, Augrabies, Northern Cape Province / by Allan Emile Saad." Thesis, Potchefstroom University for Christian Higher Education, 1987. http://hdl.handle.net/10394/606.

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Renosterkop is a large low grade tin-tungsten-zinc deposit located 85km WSW of Upington in the northern Cape Province, South Africa. The mineralization is hosted by a number of shallow-dipping, sheeted greisen bodies that are surrounded by, and partly intercalated with a well foliated granite gneiss country rock. The gneiss is taken to belong to the intrusive Riemvasmaak gneiss of the Namaqualand Metamorphic Complex. The mineralized host (referred to as TBQ) is a grey, homogeneous, fine to medium grained rock composed predominantly of quartz, biotite and topaz with minor amounts of fluorite an
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Chi, Guoxiang. "Contrôle polygénétique sur la localisation des gisements proximaux et distaux dans le champ polymétallique-stannifère à Xinlu, Guangxi, Chine méridionale /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1992. http://theses.uqac.ca.

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Naude, Karin. "A mineralogical and geochemical study of the tin deposit at NAD-mine in the Rooiberg tin field." Thesis, Stellenbosch : Stellenbosch University, 1994. http://hdl.handle.net/10019.1/58243.

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Thesis (MSc.)--Stellenbosch University, 1994.<br>ENGLISH ABSTRACT: The NAD deposit forms part of the A-Mine Complex in the Rooiberg tin field in the north-western Transvaal. Mining started in 1986 and the mine was closed recently following a decline of tin prices and metallurgical problems with ore recovery. The deposit is hosted by the Boschoffsberg Quartzite Member of the Pretoria Group sediments and is structurally controlled within the so-called Tin Zone. Extensive alteration of the original host rocks occurred during the mineralisation event. Potassic remobilisation and redistribu
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Clarke, Benjamin Paul, Cesar Lemas, Jorge Barrera, et al. "Ore Characterization and Processing Plant Remediation for a Brazilian Tin Mine." Thesis, The University of Arizona, 2017. http://hdl.handle.net/10150/624946.

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Executive Summary: To further understand the separation process used by CSN-ERSA in Brazil, ore characterization of final concentrate samples was determined through Energy Dispersive Spectroscopy (EDS) testing. Characterization of each concentrate shows a significant amount of heavy metal contamination; a result of inefficient gravity separation. CSN is looking to implement a mining method suitable for extracting ore at the Village site. The three options of mining methods are open-pit with gravel pumping, dredging, and a conveyor system. The conveyor system is recommended as the primary
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You, Tao. "Preparation and characterization of ceramic sensors for use at elevated temperatures /." View online ; access limited to URI, 2005. http://0-wwwlib.umi.com.helin.uri.edu/dissertations/dlnow/3186928.

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Bouabsa, Lakhdar. "Intrusions granitiques à albite et topaze : Minéralisations stanno-wolframifères et altérations hydrothermales associées, l'exemple du hoggar central, Algérie." Nancy 1, 1987. http://www.theses.fr/1987NAN10329.

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Le présent travail met l'accent sur la dualité du magmatisme de cette région du Hoggar Central. Outre un granite banal à biotite (parfois amphibole) constituant l'ossature principale des granites post orogéniques (Taourirts), il est mis en évidence un type particulier de granite spécialisé à albite, topaze et protolithionite comme paragénèse I. Ce magmatisme évolué est sans liaison génétique avec le précèdent comme le soulignent les contacts intrusifs marqués par des stockscheiders et les discontinuités géochimiques au niveau des éléments majeurs et tracés. La liaison spatiale et génétique des
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Yada, Marcela Midori [UNESP]. "Atributos químicos e bioquímicos em solos degradados por mineração em ecossistema amazônico em recuperação." Universidade Estadual Paulista (UNESP), 2011. http://hdl.handle.net/11449/88224.

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Made available in DSpace on 2014-06-11T19:23:10Z (GMT). No. of bitstreams: 0 Previous issue date: 2011-07-22Bitstream added on 2014-06-13T20:50:10Z : No. of bitstreams: 1 yada_mm_me_jabo.pdf: 312702 bytes, checksum: 6f892253bdb3bc5c70ef4a35150b6ce5 (MD5)<br>Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)<br>Os recursos naturais fazem da região amazônica um importante pólo para a agricultura e a exploração mineral. Entretanto, a falta de moderação na exploração causa a diminuição da matéria orgânica do solo com perda de seu potencial produtivo ou de regeneração da mata na
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Yada, Marcela Midori. "Atributos químicos e bioquímicos em solos degradados por mineração em ecossistema amazônico em recuperação /." Jaboticabal : [s.n.], 2011. http://hdl.handle.net/11449/88224.

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Orientador: Wanderley José de Melo<br>Banca: Mara Cristina Pessoa da Cruz<br>Banca: Elcio Liborio Balota<br>Resumo: Os recursos naturais fazem da região amazônica um importante pólo para a agricultura e a exploração mineral. Entretanto, a falta de moderação na exploração causa a diminuição da matéria orgânica do solo com perda de seu potencial produtivo ou de regeneração da mata nativa. A recuperação destas áreas é de fundamental importância até mesmo para a manutenção da atividade física, química e biológica do solo. O plano de recuperação das áreas degradadas iniciou em 1997, uma série de pe
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Weinhold, Günter. "Die Zinnerz-Lagerstätte Altenberg/Osterzgebirge." Sächsisches Landesamt für Umwelt und Geologie, 2002. https://slub.qucosa.de/id/qucosa%3A1426.

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Nach einem kurzen geografischen Überblick wird die fast 550-jährige Bergbaugeschichte der bedeutendsten Zinnerz-Lagerstätte des Erzgebirges dargestellt. Besondere Erwähnung findet die geologisch-lagerstättenkundliche Erforschung in den letzten 50 Jahren des ausgehenden 20. Jahrhunderts. Einer Einführung zur regionalgeologischen Position, zum Bau und zur metallogenetischen Situation des Erzfeldes folgen ausführliche Abhandlungen zur Geologie, Tektonik und Mineralisation der Lagerstätte, ebenso zu den angrenzenden Erzrevieren. Kapitel zur Rohstoffcharakteristik, Geophysik, Hydrologie/Hydrogeolog
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Moulahoum, Omar. "Dualité du magmatisme d'âge pan-africain : Aspects structuraux et pétrologiques des granites subalcalins et alumineux de la région de Tamanrasset (Hoggar central, Algérie." Nancy 1, 1988. http://www.theses.fr/1988NAN10049.

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Durant l'orogène du "Pan-Africain" (~ 600 Ma), la région du Hoggar central, à l'instar de l'ensemble du Bouclier Touareg, a été intensément affectée. Cet évènement est accompagné de la mise en place d'ensembles magmatiques variés. Dans la région de Tamanrasset, deux magmatismes de nature différente sont mis en évidence : magmatisme subalcalin et magmatisme alumineux. Le premier est représenté par les massifs syn à tardi-orogéniques (Anfeg - Tifferkit), voire post-orogénique (Aheleheg') tandis que le second est exclusivement constitué par les plutons post-orogéniques (In-Tounine et intrusions g
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Books on the topic "Tin ores"

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Good, Richard S. Gold mineralization, and tin, base metals, and thorium anomalies at Yankee Horse Ridge, Irish Creek tin area, Rockbridge County, Virginia. Commonwealth of Virginia, Dept. of Mines, Minerals, and Energy, Division of Minerals Resources, 1991.

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Ciernioch, Günter. Untersuchungen zur Aufbereitbarkeit feinkörniger thailändischer Zinnerze mit modernen Konus- und Spiralsortiersystemen: Verbesserung der Feinkornsortierung von Kassiterit. Nomos, 1987.

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Lehmann, Bernd. Metallogeny of tin. Springer-Verlag, 1990.

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Bernd, Lehmann. Metallogeny of tin. Springer-Verlag, 1990.

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Johnson, J. L. Tin and silver recovery from Coal Creek, AK. U.S. Dept. of the Interior, Bureau of Mines, 1991.

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Michniewicz, Marek. Mineralizacja cynowa w środkowej części pasma łupkowego Starej Kamienicy (Sudety zachodnie): Tin mineralization in the middle part of the Stara Kamienica schist belt (western Sudetes). Państwowy Instytut Geologiczny, 2006.

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Nyrkov, E. A. Geologo-mineralogicheskie kriterii prognoza skrytogo volʹframovogo orudenenii͡a︡ polit͡s︡iklichnoĭ skladchatoĭ oblasti T͡S︡entralʹnogo Kavkaza. Geoinformmark, 1993.

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Kopylov, M. I. Khingano-olonoĭskiĭ olovorudnyĭ raĭon: Geologo-geofizicheskie kharakteristiki, rudonosnostʹ, problemy razvitii︠a︡ syrʹevoĭ bazy. In-t tektoniki i geofiziki DO RAN, 2004.

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Warner, J. Dean. Tin occurrences near Rocky Mountain (Lime Peak), east-central Alaska. U.S. Dept. of the Interior, Bureau of Mines, 1988.

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Bray, E. A. Du. Results of grid sampling and large-scale geologic mapping for the Silsilah tin deposit. Dept. of the Interior, U.S. Geological Survey, 1985.

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Book chapters on the topic "Tin ores"

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Turner, J. F. "The Development of Methods of Treating Tin Ores in Cornwall." In Mineral Processing at a Crossroads. Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-009-4476-3_9.

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Huston, David L., Crystal Laflamme, Georges Beaudoin, and Stephen Piercey. "Light Stable Isotopes in Volcanic-Hosted Massive Sulfide Ore Systems." In Isotopes in Economic Geology, Metallogenesis and Exploration. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-27897-6_9.

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AbstractVolcanic-hosted massive sulfide (VHMS) deposits, the ancient analogues of “black smoker” deposits that currently form on the seafloor, are the products of complex mineral systems involving the interaction of seawater with the underlying volcanic pile and associated magmatic intrusions. Light stable isotopes, particularly those of oxygen, hydrogen and sulfur, have had a strong influence in determining sources of ore fluids and sulfur as well as elucidating geological processes important in the VHMS mineral systems. Oxygen and hydrogen isotope data indicate that evolved seawater was the dominant ore-forming fluid in VHMS mineral systems through geological time, although a small proportion of deposits, including high sulfidation and tin-rich deposits, may have a significant, or dominant, magmatic-hydrothermal fluid component. Higher-temperature (&gt; 200 °C) interaction of evolved seawater alters the rock pile below the seafloor, producing δ18O depletion anomalies at the deposit and district scales that can be used as a vector to ore. In contrast, lower-temperature hydrothermal alteration results in δ18O-enriched zones that commonly cap mineralized positions. An apparent decrease in the degree of high temperature 18O depletion with time may relate to the increasing importance of felsic-dominated host successions in younger deposits. δ18O anomalies have potential as an exploration tool, and have contributed directly to discovery. The other important contribution of stable isotopes to understanding the VHMS mineral system is quantification of the contribution of sulfur sources. Conventional δ34S data, when combined with Δ33S data acquired using recently developed technologies, indicate that the dominant sulfur source is igneous sulfur, either leached from the volcanic pile or introduced as a magmatic volatile (these sources are not distinguishable). The thermochemical reduction of seawater sulfate is also an important, but subordinate, sulfur source. Estimation of the proportion of seawater sulfate with geological age indicate that, on average, it has increased from 5–10% in the Archean to 20–25% in the Phanerozoic. This most likely reflects the increase in seawater sulfate contents through geological time. Although untested as an exploration tool, variations in sulfur isotope data may have utility is discriminating fertile from barren sulfide accumulations or providing vectors to ores at the deposits scale. As exploration tools, light stable isotopes suffer from a relatively high cost and slow turn-around time. If these limitations can be overcome, and new analytical methods can be developed, light stable isotopes may emerge as another tool for exploration, particularly as discoveries are made at greater depth and under cover.
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Lehmann, B. "The Stratabound Kellhuani Tin Deposits, Bolivia." In Stratabound Ore Deposits in the Andes. Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-88282-1_9.

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Villalpando, B. A. "The Tin Ore Deposits of Bolivia." In Geology of Tin Deposits in Asia and the Pacific. Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-72765-8_11.

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Voytekhovsky, Yu. "Modal Analysis of Rocks and Ores in Thin Sections." In Springer Proceedings in Earth and Environmental Sciences. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-22974-0_38.

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Wenkin, Xu, Wu Qinsheng, and Xu Junzhen. "Isotope Geochemistry of the Dachang Tin-Polymetallic Ore-Field." In Geology of Tin Deposits in Asia and the Pacific. Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-72765-8_31.

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Jun, Ye, Zhou Huaiyang, and Chen Zhugi. "On the Ore-Forming Mechanism of Some Cassiterite-Sulphide Deposits in South China." In Geology of Tin Deposits in Asia and the Pacific. Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-72765-8_19.

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Jiuling, Li, Gunther H. Moh, and Naiding Wang. "Franckeite: Mineralogical Aspects and Genetic Relations to the Dachang and Bolivian Ore Deposits." In Geology of Tin Deposits in Asia and the Pacific. Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-72765-8_30.

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Yuchuan, Chen, Huang Minzhi, Xu Yu, et al. "Geological and Metallogenic Features and Model of the Dachang Cassiterite-Sulphide Polymetallic Ore Belt, Guangxi, China." In Geology of Tin Deposits in Asia and the Pacific. Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-72765-8_26.

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Guangzhi, Tu. "Genesis of the Dachang Ore Deposit and the Formation Conditions of Cassiterite-Sulphide Deposits in General." In Geology of Tin Deposits in Asia and the Pacific. Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-72765-8_29.

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Conference papers on the topic "Tin ores"

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Repka, Vlastimil. "POSSIBILITIES OF UTILIZATION OF TAILING POND AFTER PREPARATION TIN-TUNGSTEN ORES." In 13th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/ba1.v2/s04.011.

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"HYGIENIC ANALYSIS OF ARSENIC LEVELS IN GROUNDWATER AND PUBLIC HEALTH RISK ASSESSMENT." In СОВРЕМЕННЫЕ ПРОБЛЕМЫ ЭКОЛОГИИ И ЗДОРОВЬЯ НАСЕЛЕНИЯ. ЭКОЛОГИЯ И ЗДОРОВЬЕ НАСЕЛЕНИЯ. Иркутский научный центр хирургии и травматологии, 2023. http://dx.doi.org/10.12731/978-5-98277-383-8-art20.

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The Trans-Baikal Territory territory has numerous deposits and ore occurrences of arsenic, gold, antimony. The most favorable conditions for the migration and accumulation of arsenic in groundwater are created in the zone of hypergenesis of gold-antimony and gold ore deposits, confined to chemically weakly active terrigenous rocks. In the region there is a significant technogenic component of water pollution by arsenic, due to the activities of the mining industry. In the enrichment of ores of tin, gold and other deposits with high arsenic content, the main amount of arsenic (up to 80 % and mo
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Reeves, Nigel, Gordon H. John, and Bob Major. "Evaluation and Potential Remediation of the Industrial Norm Legacy in Liverpool." In ASME 2009 12th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2009. http://dx.doi.org/10.1115/icem2009-16096.

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Sefton, on the north side of Liverpool, holds a radioactive legacy from its industrial past. This legacy is in the form of Tin slag buried in sub-surface seams. Located near the docks and adjacent to the rich Lancashire coal seams, Sefton became one of the main production centres of Tin plate in Britain. A consequence of this industrial process is the production of mildly radioactive waste slag. Tin rich ores are heated under reducing conditions to produce a molten metal stream This is then separated into the component metal streams. Solid wastes produced by this process are known as slag and
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Subandrio, Riskaviana Kurniawati, Wiwik Dahani, and Shima Parameswari Adji. "Optimization of tin ore concentration using gravity method." In 4TH INTERNATIONAL CONFERENCE ON EARTH SCIENCE, MINERAL AND ENERGY. AIP Publishing, 2023. http://dx.doi.org/10.1063/5.0146309.

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Cui, Chuanfa, Shuming Wen, Yawei Liu, and Yijie Wang. "Recovery copper and tin from a complex Oxide Copper Ore." In 2015 2nd International Conference on Machinery, Materials Engineering, Chemical Engineering and Biotechnology. Atlantis Press, 2016. http://dx.doi.org/10.2991/mmeceb-15.2016.43.

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Jia, Fuju, Wu Wei, Hongliang Nian, and Zize Xiao. "Application of Geostatistics in the Study of Ore-controlling Factors : Taking Example of Manjiazhai Ore Segment in Dulong Tin Polymetallic Ore Deposit." In 2015 International Conference on Materials, Environmental and Biological Engineering. Atlantis Press, 2015. http://dx.doi.org/10.2991/mebe-15.2015.30.

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Anfaresi, Shofi, Intan Putri, Ridho Mulia, Anisa Alfisyahr, and Nurul Muzayyanah. "Bangka’s Tin Sea Sand-Fe3O4 as A Removal of Heavy Metals in By-Product of Tin Ore Processing." In Proceedings of the International Conference on Maritime and Archipelago (ICoMA 2018). Atlantis Press, 2019. http://dx.doi.org/10.2991/icoma-18.2019.7.

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Yang, Yongqiang, Yang Wang, and Yufen Zhang. "Ore-Forming Fluids Evolution on the Weilasituo Tin Deposit, Inner Mongolia, China." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.3009.

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Borchert, Manuela, Pilar Valsera Moreno, Max Wilke, et al. "Tin transport in ore fluids - in-situ insight from cassiterite dissolution experiments." In Goldschmidt2022. European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10072.

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Zhang, Daiyun, Hongbo Li, Guoxin Zhang, Yuliang Wang, and Weizhe Zhang. "Determination of Tungsten Trioxide Content in Tungsten Tin Ore by Gravimetric Method." In Proceedings of The 11th Academic Conference of Geology Resource Management and Sustainable Development. Aussino Academic Publishing House, 2023. http://dx.doi.org/10.52202/073371-0049.

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Reports on the topic "Tin ores"

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Ostersetzer-Biran, Oren, and Alice Barkan. Nuclear Encoded RNA Splicing Factors in Plant Mitochondria. United States Department of Agriculture, 2009. http://dx.doi.org/10.32747/2009.7592111.bard.

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Mitochondria are the site of respiration and numerous other metabolic processes required for plant growth and development. Increased demands for metabolic energy are observed during different stages in the plants life cycle, but are particularly ample during germination and reproductive organ development. These activities are dependent upon the tight regulation of the expression and accumulation of various organellar proteins. Plant mitochondria contain their own genomes (mtDNA), which encode for a small number of genes required in organellar genome expression and respiration. Yet, the vast ma
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Boily-Auclair, É., P. Mercier-Langevin, P. S. Ross, and D. Pitre. Alteration and ore assemblages of the LaRonde Zone 5 (LZ5) deposit and Ellison mineralized zones, Doyon-Bousquet-LaRonde mining camp, Abitibi, Quebec. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329637.

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The LaRonde Zone 5 (LZ5) mine is part of the Doyon-Bousquet-LaRonde mining camp and is located in the southern part of the Abitibi greenstone belt in northwestern Quebec. The LZ5 deposit consists of three stacked mineralized corridors: Zone 4, Zone 4.1, and Zone 5. Zones 4 and 4.1 are discontinuous satellite mineralized corridors, whereas Zone 5 represents the main mineralized body. The mineralized zones of the LZ5 deposit and adjacent Ellison property (Ellison A and B zones) are hosted in the strongly-deformed, 2699-2695 Ma transitional to calcalkaline, intermediate to felsic, volcanic and vo
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