Bibliografías temáticas / Mineralogy, geochemistry, Kalgoorlie, gold

Literatura académica sobre el tema "Mineralogy, geochemistry, Kalgoorlie, gold"

Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 19 de febrero de 2022

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Artículos de revistas sobre el tema "Mineralogy, geochemistry, Kalgoorlie, gold"

Mueller, Andreas G. y Janet R. Muhling. "Early pyrite and late telluride mineralization in vanadium-rich gold ore from the Oroya Shoot, Paringa South mine, Golden Mile, Kalgoorlie: 3. Ore mineralogy, Pb-Te (Au-Ag) melt inclusions, and stable isotope constraints on fluid sources". Mineralium Deposita 55, n.º 4 (16 de abril de 2019): 733–66. http://dx.doi.org/10.1007/s00126-019-00876-6.

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Weinberg, Roberto F. y Peter van der Borgh. "Extension and gold mineralization in the Archean Kalgoorlie Terrane, Yilgarn Craton". Precambrian Research 161, n.º 1-2 (febrero de 2008): 77–88. http://dx.doi.org/10.1016/j.precamres.2007.06.013.

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Harris, D. C. "The Mineralogy of gold and its relevance to gold recoveries". Mineralium Deposita 25, S1 (diciembre de 1990): S3—S7. http://dx.doi.org/10.1007/bf00205243.

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Bateman, Roger y Frank P. Bierlein. "On Kalgoorlie (Australia), Timmins–Porcupine (Canada), and factors in intense gold mineralisation". Ore Geology Reviews 32, n.º 1-2 (septiembre de 2007): 187–206. http://dx.doi.org/10.1016/j.oregeorev.2006.08.001.

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Wilson, G. C. y J. C. Rucklidge. "Mineralogy and microstructures of carbonaceous gold ores". Mineralogy and Petrology 36, n.º 3-4 (julio de 1987): 219–39. http://dx.doi.org/10.1007/bf01163261.

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Shatalov, M. M. "GOLD OF THE DEPTHS OF UKRAINE. GENERAL INFORMATION, GEOCHEMISTRY AND MINERALOGY OF GOLD". Visnik Nacional'noi' academii' nauk Ukrai'ni, n.º 07 (20 de julio de 2020): 16–26. http://dx.doi.org/10.15407/visn2020.07.016.

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Sergeev, N. B. y D. J. Gray. "Gold mass balance in the regolith, Mystery Zone, Mt Percy, Kalgoorlie, Western Australia". Geochemistry: Exploration, Environment, Analysis 1, n.º 4 (noviembre de 2001): 307–12. http://dx.doi.org/10.1144/geochem.1.4.307.

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Vaughan, J. P. y A. Kyin. "Refractory gold ores in Archaean greenstones,Western Australia: mineralogy, gold paragenesis, metallurgical characterization and classification". Mineralogical Magazine 68, n.º 2 (abril de 2004): 255–77. http://dx.doi.org/10.1180/0026461046820186.

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AbstractMesothermal gold ores in the Archaean Yilgarn Craton of Western Australia are dominated by a pyrite ± arsenopyrite ± pyrrhotite sulphide assemblage. Many of these ores are refractory to varying degrees and require treatment by roasting, bacterial oxidation or finer milling. The most common sulphide ore types can be sub-divided broadly into pyritic (pyrite±pyrrhotite) and arsenical types (pyrite+arsenopyrite± pyrrhotite). Arsenical ores vary from highly refractory to free-milling. Arsenopyrite in highly refractory ores is finer grained, As-deficient (27 –32.5 at.% As), contains high average concentrations of submicroscopic gold (60 –270 ppm), but does not contain inclusions of particulate gold. Arsenopyrite in free-milling ores is coarser grained, less As-deficient to slightly As-rich (30 –35 at.% As), contains low or negligible concentrations of submicroscopic gold, but contains inclusions and fracture fillings of particulate gold. In some refractory arsenical ores, pyrite also contains moderately high levels of submicroscopic gold (20 –40 ppm), the concentration of which is directly related to As content of the pyrite.Pyritic ores are free-milling to mildly refractory, or rarely moderately refractory. Pyrite in pyritic ores contains negligible to low levels of submicroscopic gold (<5 ppm). Other reasons for refractory behaviour in pyritic ores include very fine-grained native gold inclusions in pyrite, or the presence of gold-bearing tellurides.It is concluded that submicroscopic gold is incorporated into the crystal lattices of arsenopyite and arsenical pyrite at sub-greenschist to lower greenschist-facies temperatures, and is progressively expelled as inclusions and fracture fillings of native gold in sulphides, and ultimately into the gangue, as recrystallization proceeds through upper greenschist- into amphibolite-facies temperatures, during deformation and burial. Submicroscopic gold is expelled more rapidly from pyrite than arsenopyrite.Pyrrhotite progressively replaces primary pyrite at higher temperatures, but rarely contains gold. Finally, a metallurgical classification scheme for refractory ores is presented which incorporates the above mineralogical conclusions.

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Kuleshevich, L. V. y V. Ya Gor’kovets. "Mineralogy of the Precambrian southern Kostomuksha gold prospect in Karelia". Geology of Ore Deposits 50, n.º 7 (diciembre de 2008): 599–608. http://dx.doi.org/10.1134/s1075701508070118.

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Ying, Jifeng, Xinhua Zhou, Shengrong Li y Daisheng Sun. "Genetic mineralogy of pyrite from Jindoushan gold deposit, Yantai, Shandong Province". Chinese Journal of Geochemistry 20, n.º 3 (septiembre de 2001): 219–25. http://dx.doi.org/10.1007/bf03166142.

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Tesis sobre el tema "Mineralogy, geochemistry, Kalgoorlie, gold"

Salem, Hanaa Mahmoud. "Geochemistry, mineralogy, and genesis of the Copperstone gold deposit, La Paz County, Arizona". Diss., The University of Arizona, 1993. http://hdl.handle.net/10150/186423.

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Copperstone is a mid-Tertiary "detachment gold" deposit that is herein classified as a new subtype of epithermal deposit. Copperstone is similar to many active geothermal systems in terms of host lithology, temperature, and related siliceous alteration mineralogy, except in the hypogene oxide assemblages, the high salinity, and the lack of sulfides and the pathfinder toxic elements. The host rock is mainly Jurassic quartz latite porphyry and Tertiary sedimentary breccias. Early stages of alteration were K-metasomatic and propylitic, and alteration that accompanied gold mineralization was mainly chloritization and silicification. Mineralization is structurally controlled and is restricted along the Copperstone Listric Fault with minor mineralization along high-angle NE and NW faults, as with many other deposits in west-central Arizona. The gold stage of mineralization was superimposed on previously K-metasomatized rocks. Hypogene mineralization can be divided into 3 paragenetic stages: early amethyst-quartz-Fe-rich-chlorite-specularite-hematite-Au° of stage C; late-stage fine-grained euhedral quartz-adularia-chrysocolla ± malachite ± magnetite ± chalcopyrite-pink fluorite-barite-ankerite-calcite-Au° of stage D; and barren quartz-pale green fluorite-barite-calcite-hematite of stage E. Gold occurs as free particles or is encapsulated in amethyst and late fine-grained euhedral quartz. The time of mineralization is Miocene or younger and the depth of mineralization was 1 Km. Gold mineralization was related to boiling such that a hot spring system did operate at Copperstone. Copperstone is a hydrothermal system created during the last stages of detachment faulting, with mineralization controlled by boiling, and "second boiling" was the principal trigger of Copperstone gold deposition in an environment of falling temperatures and pressures on chloride-rich brine fluids. Variation in δ³⁴S indicates that two different fluids are involved in this system, and that a deeper, "lighter" hydrothermal fluid mixed with a "heavier" basin brine. δ¹⁸O values from carbonates confirm the extent of isotopic exchange with an aqueous reservoir and indicates that oxidation accompanied gold deposition.

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Munro-Smith, Vera. "Chemical mineralogy of cobalt and gold in the Mt Isa block /". View thesis, 1998. http://library.uws.edu.au/adt-NUWS/public/adt-NUWS20030826.124022/index.html.

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Thesis (M. Sc.) (Hons.) -- University of Western Sydney, Nepean, 1998.
Thesis submitted for the degree of Master of Science (Honours) in the University of Western Sydney. Bibliography : p. 100-105.

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Burke, Michelle Lynn. "An Electron Microscopy Investigation of Gold and Associated Minerals from Round Mountain, Nevada". Miami University / OhioLINK, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=miami1438354504.

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Green, Bradley. "A study of the Wilkins and Green and Gold Copper-gold prospects, Olary Block, South Australia with emphasis on petrology, geochemistry and ore mineralogy /". Title page, contents and abstracts only, 1996. http://web4.library.adelaide.edu.au/theses/09SB/09sbg811.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1998.
Australian National Grid Reference (SI 54-2) 1:250 000. Four folded maps in pocket pasted onto back cover. Includes bibliographical references (leaves 62-68).

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Bourdeau, Julie. "Petrology, Mineralogy and Geochemistry of the Beattie Syenite and Country Rocks, Abitibi Greenstone Belt, Québec". Thèse, Université d'Ottawa / University of Ottawa, 2013. http://hdl.handle.net/10393/26201.

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The Beattie syenite is composed of a series of lenticular bodies of syenitic rocks, situated immediately north of the Porcupine-Destor fault zone in the town of Duparquet, approximately 32 km north of Rouyn-Noranda in the Abitibi Subprovince. The principal body is 3.3 km long and 470 m in width and is flanked by a series of smaller lenses to the south and northeast. The intrusion has been zircon dated at 2682±1Ma and 2682.9±1.1 Ma and hosted the major part of the Au-mineralization of the now defunct Beattie mine, which was an important producer of gold in the area from 1933 to 1956 (9.66 Mt at 4.88 g/t Au). A total of 5 petrographic units are defined here, on the basis of field relationships, macroscopic textures, petrology and mineralogy: 1- The porphyritic Beattie syenite unit is composed of 2% to 10% of tabular sub- to anhedral feldspar phenocrysts about 2 mm to 10 mm in size, set in a red feldspathic and aphanitic matrix. This unit can be strongly cataclastic with abundant hydrothermal minerals. 2- The equigranular magnetite-bearing syenite unit includes few feldspar phenocrysts, about 2 mm to 10 mm in a fine-grained matrix. It is characterized by unaltered titanite, epidote, hornblende porphyroblasts and is the only unit with actinolite replacing clinopyroxene. 3- The porphyritic Central Duparquet syenite unit contains between 2% - 25% of coarse equant euhedral feldspar phenocrysts, about 5 mm to 16 mm in size, in a red or sometimes grey aphanitic matrix. 4- The megaporphyritic syenite unit is composed of very coarse alkali feldspar phenocrysts, typically 1 cm to 6 cm across, in a red aphanitic matrix. The phenocrysts often form a glomeroporphyritic texture. 5- The lath syenite unit occurs as numerous ~m-width thin dykes, which cross-cut all other petrographic units. These dykes display a characteristic trachytic texture, as defined by the preferential alignment of alkali feldspar laths, which are typically 1 cm to 3 cm in a grey or red aphanitic matrix. Petrology and geochemistry investigations revealed that the syenite intruded into the older 2720-2718 Ma volcanic Deguisier Formation and the <2687±2 Ma sediments of the Porcupine Group. Detailed geochemical analysis revealed that the Deguisier Formation is composed of three units, forming a complete tholeiitic suite. The Deguisier Formation is proposed here to have been produced in a volcanic arc setting. Detailed petrological, mineralogical and geochemical studies indicate that, the syenite is part of the alkaline series and is metaluminous to peraluminous. The syenite intruded at shallow depths through a sequence of injections, yielding the five comagmatic units. The syenite and country rocks were then subjected to a series of hydrothermal alterations and brittle deformation events, combined with metamorphism to the greenschist facies. The Au-mineralization in this region is attributed to the hydrothermal alteration with brittle deformation.

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Moss, Roger. "Geochemistry and mineralogy of gold in the PACMANUS and Susu knolls hydrothermal systems, eastern Manus basin, Papua New Guinea". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0020/NQ53744.pdf.

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Törmänen, T. (Tuomo). "Ore mineralogy, geochemistry, and formation of the sediment-hosted sea floor massive sulfide deposits at Escanaba Trough, NE Pacific, with emphasis on the transport and deposition of gold". Doctoral thesis, University of Oulu, 2004. http://urn.fi/urn:isbn:9514276264.

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Abstract Recent sea floor sulfide deposits form when seawater, heated within the oceanic crust, discharges to the sea floor. Upon mixing with cold seawater, sulfide-forming elements such as sulfur, iron, copper, and zinc are precipitated from the fluid. Actively forming sea floor massive sulfide deposits are found from different lithologic and tectonic environments varying from mid-ocean ridges to back-arc spreading centers. At a few localities, sulfide deposits are associated with turbiditic sediments that cover the axial valley of the spreading center. The southern part (Escanaba Trough) of the Gorda Ridge (NE Pacific) is one such example. At Escanaba Trough, massive sulfide deposits are associated with small sediment hills, which were uplifted by the intrusion of sills and laccoliths within the sediments. Hydrothermal deposits are dominated by pyrrhotite-rich massive sulfides, with subordinate amounts of sulfate-rich precipitates and polymetallic sulfides. Compared to deposits hosted by volcanites, Escanaba Trough sulfides contain relatively low amounts of copper and zinc. However, the average gold concentration is relatively high for a sediment-hosted deposit, and is comparable with other, Au-enriched, sea floor sulfide deposits. Despite the relatively high Au concentration in many volcanic-hosted sea floor sulfide deposits, discrete Au grains are rare. They occur mostly with sphalerite, pyrite, chalcopyrite and tetrahedrite-tennantite. Sixteen of the pyrrhotite-rich samples from Escanaba Trough were found to contain visible Au grains. They occur mostly with native Bi and various BiTe phases, and to lesser degree, with Fe-Co sulfarsenides. Transport of Au in sea floor hydrothermal systems is attributed to the presence of Au(HS)2- complex, which is destabilized when the fluid mixes with seawater. Hydrothermal fluids are generally undersaturated with respect to Au complexes and additional mechanisms, such as remobilizing earlier precipitated Au is required to explain the high Au concentrations encountered in many deposits. At Escanaba Trough the mechanism is attributed to early precipitation of Bi as melt droplets, at temperatures greater its melting temperature, as liquid Bi is capable of collecting Au even from an undersaturated fluid. Upon cooling Au is exsolved from the Bi host as native Au or maldonite (Au2Bi).

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Taylor, Mackenzie C. "GOLD FROM THE TYPE 4 ORE OF ROUND MOUNTAIN, NEVADA: A TEXTURAL AND MINERALOGICAL STUDY OF MACROCRYSTALLINE GOLD VS. DISSEMINATED GOLD". Miami University / OhioLINK, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=miami1512407677037903.

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Zoller, Kevin M. "Porphyritic Intrusions of the Helen Zone in the Cove Deposit, Lander County, Nevada". University of Akron / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=akron1398079611.

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Olivo, Gema Ribeiro. "Les gites d'or palladifères des mines de Caue et de Conceicao, dans les formations de fer du type lac Supérieur du district d'Itabira, Craton Sao Francisco, Bresil : structure, minéralogie, géochronologie et métallogenie = (Palladium-bearing gold deposits of the caue and conceicao mines, hosted by lake superior-type iron-formations of the Itabira district, Sao Francisco craton, Brazil : structure, mineralogy, geochronology and metallogeny) /". Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1994. http://theses.uqac.ca.

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Libros sobre el tema "Mineralogy, geochemistry, Kalgoorlie, gold"

Nekrasov, I. I︠A︡. Geochemistry, mineralogy and genesis of gold deposits. Rotterdam: A.A. Balkema, 1996.

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The mineralogy and geochemistry of the Hemlo gold deposit, Ontario. Ottawa, Canada: Energy, Mines and Resources Canada, 1989.

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Warmada, I. Wayan. Ore mineralogy and geochemistry of the Pongkor epithermal gold-silver deposit, Indonesia. Clausthal-Zellerfeld: Papierflieger Verlag GmbH, 2003.

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Warmada, I. Wayan. Ore mineralogy and geochemistry of the Pongkor epithermal gold-silver deposit, Indonesia. Clausthal-Zellerfeld: Papierflieger, 2003.

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G, Mironov A., Shcherbakov I͡U︡riĭ Gavrilovich y Buri͡a︡tskiĭ geologicheskiĭ institut, eds. Geokhimii͡a︡ zolota v ėndogennykh prot͡s︡essakh i uslovii͡a︡ formirovanii͡a︡ zolotorudnykh mestorozhdeniĭ. Novosibirsk: "Nauka", 1992.

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International Symposium on Applied Mineralogy (1989 Montreal, Quebec). Process Mineralogy IX: Applications to mineral beneficiation, metallurgy, gold, diamonds, ceramics, environment, and health : proceedings of International Symposium on Applied Mineralogy (MAC-ICAM-CAM) held at Montreal, Quebec, Canada on May 14 to 17, 1989, and of the Process Mineralogy Symposium held at Las Vegas, Nevada, February 27 to March 2, 1989 ... Warrendale, Pa: Minerals, Metals & Materials Society, 1990.

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Dodin, D. A. Platinometallʹnye mestorozhdenii︠a︡ mira. Moskva: OOO "Geoinformt︠s︡entr,", 2003.

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Razin, L. V. Promyshlenno-perspektivnyĭ mineralʹno-syrʹevoĭ potent︠s︡ial Uralʹskogo platinonosnogo poi︠a︡sa: (voprosy geologii, mineralogii, geokhimii platiny, platinoidov, poputnogo zolota i tekhnologii obogashchenii︠a︡ platinovometallʹnykh rud i rossypeĭ) = Future commercial production and mineral resource potential of the Urals platinum bearing belt (issues of geology, mineralogy, geochemistry of platinum, platinoids, associated gold and technology for concentration of platinum metal ores and placers. Moskva: Universitetskai︠a︡ kniga, 2008.

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Geochemistry Mineralogy & Genesis Gol. Taylor & Francis, 1996.

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Nekrasov, I. Y. Geochemistry, Mineralogy and Genesis of Gold Deposits. CRC Press LLC, 2018.

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Capítulos de libros sobre el tema "Mineralogy, geochemistry, Kalgoorlie, gold"

Fu, Kaibin, Shu Chen, Zhen Wang, Junhui Xiao y Deqiang Luo. "Lime-Assisted Cyanide Leaching of Refractory Gold Ores from Ajialongwa Mine". En Springer Geochemistry/Mineralogy, 107–13. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_12.

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Cheng, Yunhong, Fei Huang, Guanglu Li, Qingyu Yang, Han Peng y Rui Liu. "Analyzing the Characteristics and Available Attributes of Skarn Gold Deposit Tailings". En Springer Geochemistry/Mineralogy, 51–58. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_6.

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Ulsen, Carina, Henrique Kahn, Guilherme Nery, Daniel Uliana y Juliana L. Antoniassi. "Gold Characterization by MLA and Technological Tests: Discussion of Sample Preparation and Results". En Springer Geochemistry/Mineralogy, 39–49. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_5.

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Baibatsha, Adilkhan, Kulyash Dyussembayeva y Aimkhan Kassenova. "Microparagenetic Associations of Gold in Ore-Forming Minerals from Deposits of Different Geological and Industrial Types of Kazakhstan". En Springer Geochemistry/Mineralogy, 1–8. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_1.

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Morteani, G. "Mineral Economics, Mineralogy, Geochemistry and Structure of Gold Deposits: An Overview". En Prehistoric Gold in Europe, 97–113. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-015-1292-3_9.

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Nekrasov, I. Ya. "Mineralogy of Gold". En Geochemistry, Mineralogy and Genesis of Gold Deposits, editado por Margaret Majithia, 69–120. Routledge, 2018. http://dx.doi.org/10.1201/9780203753651-3.

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Nekrasov, I. Ya. "Systematisation of Gold Deposits". En Geochemistry, Mineralogy and Genesis of Gold Deposits, editado por Margaret Majithia, 1–36. Routledge, 2018. http://dx.doi.org/10.1201/9780203753651-1.

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Nekrasov, I. Ya. "Geochemical Characteristics of Gold". En Geochemistry, Mineralogy and Genesis of Gold Deposits, editado por Margaret Majithia, 37–68. Routledge, 2018. http://dx.doi.org/10.1201/9780203753651-2.

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Nekrasov, I. Ya. "Solubility of Gold in Chloride Solutions and Genesis of Gold-Quartz Deposits". En Geochemistry, Mineralogy and Genesis of Gold Deposits, editado por Margaret Majithia, 121–40. Routledge, 2018. http://dx.doi.org/10.1201/9780203753651-4.

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Nekrasov, I. Ya. "Genetic Features of Gold Deposits". En Geochemistry, Mineralogy and Genesis of Gold Deposits, editado por Margaret Majithia, 264–306. Routledge, 2018. http://dx.doi.org/10.1201/9780203753651-8.

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Informes sobre el tema "Mineralogy, geochemistry, Kalgoorlie, gold"

Harris, D. C. The mineralogy and geochemistry of the Hemlo Gold Deposit, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127237.

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Lauzon, M. C., P. Mercier-Langevin, G. Beaudoin, O. Côté-Mantha, M. Simard, M. Valette y S. De Souza. Mineralogy and geochemistry of the Whale Tail Zone, Amaruq gold project, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/300659.

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Peter, J. M. y S. D. Scott. Mineralogy and Geochemistry of the Windy Craggy Copper - Cobalt - Gold Massive Sulphide Deposit, northwestern British Columbia Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132328.

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Plouffe, A. Geochemistry, lithology, mineralogy, and visible gold grain content of till in the Manson River and Fort Fraser map areas, central British Columbia (NTS 93 K and N). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205745.

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Geochemistry, geochronology, mineralogy, and geology suggest sources of and controls on mineral systems in the southern Toquima Range, Nye County, Nevada; with geochemistry maps of gold, silver, mercury, arsenic, antimony, zinc, copper, lead, molybdenum, bismuth, iron, titanium, vanadium, cobalt, beryllium, boron, fluorine, and sulfur; and with a section on lead associations, mineralogy and paragenesis, and isotopes. US Geological Survey, 2003. http://dx.doi.org/10.3133/mf2327c.

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