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Статті в журналах з теми "Ore geochemistry"
de Boorder, H. "Geochemistry of sedimentary ore deposits." Earth-Science Reviews 22, no. 3 (November 1985): 241–42. http://dx.doi.org/10.1016/0012-8252(85)90063-7.
Повний текст джерелаWolf, Karl H. "Geochemistry of sedimentary ore deposits." Chemical Geology 48, no. 1-4 (March 1985): 355–59. http://dx.doi.org/10.1016/0009-2541(85)90058-0.
Повний текст джерелаRidge, J. D. "Geochemistry of sedimentary ore deposits." Sedimentary Geology 44, no. 1-2 (May 1985): 176–78. http://dx.doi.org/10.1016/0037-0738(85)90041-7.
Повний текст джерелаPrice, Jonathan G. "SEG Presidential Address: I Never Met a Rhyolite I Didn’t Like – Some of the Geology in Economic Geology." SEG Discovery, no. 57 (April 1, 2004): 1–13. http://dx.doi.org/10.5382/segnews.2004-57.fea.
Повний текст джерелаLandais, P. "Organic geochemistry of sedimentary uranium ore deposits." Ore Geology Reviews 11, no. 1-3 (June 1996): 33–51. http://dx.doi.org/10.1016/0169-1368(95)00014-3.
Повний текст джерелаZamana, L., and L. Taskina. "GEOCHEMISTRY OF DRAINAGE WATER OF GOLD-ORE DEPOSITS OF DARASUN ORE FIELD." Postgraduate. Supplement to “Transbaikal State University Journal” 12, no. 2 (2018): 41–47. http://dx.doi.org/10.21209/2074-9155-2018-12-2-41-47.
Повний текст джерелаPavlenko, Yu. "Predictive geochemistry of ore gold in Eastern Transbaikalia." Transbaikal State University Journal 26, no. 10 (2020): 6–14. http://dx.doi.org/10.21209/2227-9245-2020-26-10-6-14.
Повний текст джерелаPeng, 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 (December 1, 1999): 125–51. http://dx.doi.org/10.1127/njma/175/1999/125.
Повний текст джерелаTornos, Fernando, and Daniel Arias. "Sulphur and lead isotope geochemistry of the Rubiales Zn-Pb ore deposit (NW Spain)." European Journal of Mineralogy 5, no. 4 (July 22, 1993): 763–74. http://dx.doi.org/10.1127/ejm/5/4/0763.
Повний текст джерелаSmith, M. "Geochemistry of Skarn and Ore Formation in Dolomites." Mineralogical Magazine 63, no. 4 (1999): 613–14. http://dx.doi.org/10.1180/minmag.1999.063.4.07.
Повний текст джерелаДисертації з теми "Ore geochemistry"
Lundkvist, Anders. "The process water geochemistry of the Kiirunavaara magnetite ore." Licentiate thesis, Luleå tekniska universitet, 1998. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-26157.
Повний текст джерелаUnger, Derick Lee Saunders James A. Hames W. "Geochronology and geochemistry of Mid-Miocene Bonanza low-sulfidation epithermal ores of the northern Great Basin, USA." Auburn, Ala, 2008. http://repo.lib.auburn.edu/EtdRoot/2008/SPRING/Geology_and_Geography/Thesis/Unger_Derick_6.pdf.
Повний текст джерелаTanner, Dominique. "In situ mineral geochemistry as a guide to ore-forming processes." Phd thesis, Canberra, ACT : The Australian National University, 2014. http://hdl.handle.net/1885/125140.
Повний текст джерелаSharman, Elizabeth. "Application of multiple sulfur isotope analysis to Archean ore-forming processes." Thesis, McGill University, 2011. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=104747.
Повний текст джерелаL'identification des sources de soufre dans la minéralisation est importante car elle permet de comprendre les processus et de définir la meilleure méthode d'exploration. Elle peut aussi aider à la compréhension de la chimie des océans et de l'atmosphère lors de sa formation. Le fractionnement indépendant de la masse des isotopes du soufre dans l'atmosphère de l'Archéen fournit une emprunte unique permettant d'identifier les sources de soufre non magmatiques. La nature chimique conservatrice des signatures du Δ33S en fait un outil puissant pour la déconvolution des processus minéralisateurs Archéen.Cette thèse présente trois applications de l'analyse multiple des isotopes du soufre dans l'investigation des processus de minéralisation à l'Archéen. La première étude teste les modèles de formation des sulfures massifs volcanogènes (SMV) Néo- et Mésoarchéen récemment proposés ne requérant peu ou pas d'apport de sulfate marin par rapport aux systèmes SMV du Phanérozoïque et contemporains où le sulfate marin joue un rôle important. Ces modèles sont réévalués en utilisant le camp de Noranda (~2.7 Ga), sous-province de l'Abitibi, et en combinant l'utilisation de données provenant de l'analyse des isotopes du soufre et des éléments traces.Les sulfures analysés pour cette étude ont des valeurs de δ34SV-CDT entre -14.90 et +2.49 ‰, et des valeurs de Δ33SV-CDT entre -0.59 et -0.03 ‰. Selon notre interprétation, les valeurs négatives de Δ33S sont dues à l'incorporation de soufre provenant de l'eau de mer. La proportion de soufre marin aurait augmenté durant l'affaissement et l'évolution subséquente de la caldera de Noranda. Des concentrations plus élevées de Se combinées à des valeurs près de 0 ‰ et d'un haut ratio Fe/(Fe + Zn) dans les sphalérites indiquent une température de formation élevée.La deuxième étude est une investigation des sources de soufre ayant contribuées à la formation des SMV riches en Cu et en Au du camp minier Doyon-Bousquet-LaRonde (DBL; ~2.7 Ga), aussi dans la sous-province de l'Abitibi. Une source magmatique-hydrothermale de fluides minéralisateurs importante était l'interprétation donnée pour ce sous-groupe. À l'exception d'une lentille mineure, l'analyse isotopique multiple des dépôts du camp minier DBL indiquent clairement une affinité ignée-magmatique (Δ33SV-CDT = 0.14 to +0.04 ‰), avec peu ou pas de contribution de soufre provenant de la surface. Par contre, les sulfures formés sur le plancher océanique ou près de celui-ci exhibe une contribution distinctive des sulfates marins (Δ33SV-CDT = 1.43 to 0.34 ‰). D'un autre côté, l'absence de variation des valeurs du Δ33S entre des lentilles minéralisées avec une altération alumineuse et celles ne démontrant pas cette altération remet en question les l'identification des dépôts de type SMV ayant une contribution importante ou dominante de fluides magmatiques. La dernière étude examine les sources de soufre du Platreef – horizon riche en éléments du groupe platine (EGP) du flanc nord du Complexe Igné Bushveld (CIB) en Afrique du Sud. Le Platreef contient un haut pourcentage de sulfures par rapport au dépôt analogue Merensky Reef des flancs est et ouest du CIB. Il est en contact direct avec les sédiments Néoarchéens à Paléoprotérozoïques qui sont une source potentielle de soufre locale. D'un autre côté, les analyses du Δ33S des sulfures du Platreef permettent d'identifier une contribution de soufre hétérogène provenant de la croûte terrestre, avant et après la mise en place du gisement.Cette étude démontre clairement que l'analyse multiple des isotopes du soufre est un outil puissant dans l'identification des sources de soufre des processus minéralisateurs de l'Archéen, ainsi que ceux impliquant des roches archéennes, et cette approche peut être appliquée à un éventail de problèmes et types de dépôt. Aussi, elle soulève des questions importantes sur le rôle du sulfate marin dans la formation des dépôts SMV de l'Archéen et les caractéristiques du magma du CIB.
Archibald, Sandy M. "The role of vapour in the transport and deposition of metals in ore-forming systems /." Thesis, McGill University, 2002. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=82821.
Повний текст джерелаCalculations based on the solubility data indicate an economic high-sulphidation Au deposit (e.g., Nansatsu, Japan; 36 tonnes) could form in ~30,000 years, whereas a porphyry copper deposit (e.g., 50 million tonnes at 0.5% Cu) could form in as little as ~20,500 years, assuming transport only in the vapour phase.
Precious- and base-metal-rich composite scales, containing up to 111 ppm Au and 628 ppm Ag, occur in surface pipes at the Momotombo geothermal field, Nicaragua. Polysulphide scale fragments, comprising chalcopyrite, sphalerite, galena, electrum and hessite grains in a matrix of amorphous silica, formed as a result of cooling and ligand loss induced by boiling, during fluid ascent in well MT-36. Secondary bornite, stromeyerite and chalcocite/digenite replaced chalcopyrite through the addition of Cu and Ag and an increase in fO2 . A drop in pH due to well closure resulted in replacement of primary and secondary sulphides by tetrahedrite.
Reaction-path modelling using the program CHILLER simulates deposition of minerals from the reconstructed deep geothermal fluid, at temperature intervals (depths) along excess enthalpy and isoenthalpic boiling paths. These simulations accurately reproduce the paragenetic sequence of base- and precious-metal mineralization in the scales. The modelling indicates excess enthalpy boiling results in metal precipitation at greater depths than would be expected for isoenthalpic boiling, and that at Momotombo this occurs through the destabilisation of bisulphide complexes in response to loss of CO2 and H2 S during phase separation.
Jiang, Shao-Yong. "Chemical and boron isotopic compositions of tourmaline from sedex-type and metaevaporite ore deposits." Thesis, University of Bristol, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.294950.
Повний текст джерелаWay, Bryan C. "Geology and Geochemistry of Sedimentary Ferromanganese Ore Deposits, Woodstock, New Brunswick, Canada." Thesis, Fredericton: University of New Brunswick, 2012. http://hdl.handle.net/1882/44600.
Повний текст джерелаLevitan, Denise Madeline. "Statistical Analysis of the Environmental Geochemistry of an Unmined Uranium Ore Deposit." Diss., Virginia Tech, 2014. http://hdl.handle.net/10919/64782.
Повний текст джерелаPh. D.
Meadows, Holly Rachael. "Mineral Geochemistry, Deformation and Ore Fluid Evolution in the Capricorn Orogen, WA." Thesis, Curtin University, 2017. http://hdl.handle.net/20.500.11937/69391.
Повний текст джерелаRempel, Kirsten U. "The solubility and speciation of molybdenum in water vapour at elevated temperatures and pressures : implications for ore genesis." Thesis, McGill University, 2004. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=82411.
Повний текст джерелаCalculations based on the extrapolated solubility of MoO 3 in equilibrium with molybdenite at 600ºC and 500 bars, using average H2O and total S fluxes of actively degassing volcanoes, with fO2 and fS2 controlled by the assemblage hematite-magnetite-pyrite, indicate that the vapour phase can transport sufficient Mo in about 900,000 years (within the life of some geothermal systems) to form a deposit of 336 Mt, with an average grade of 0.087% Mo (e.g., the Endako Mo-porphyry deposit, Canada).
Книги з теми "Ore geochemistry"
Stanton, R. L. Ore elements in arc lavas. Oxford: Clarendon Press, 1994.
Знайти повний текст джерелаNash, J. Thomas. Geochemical signatures of ore deposits and mineralized rocks in the Cedar Mountains, Mineral and Nye Counties, Nevada. [Reston, Va.?]: U.S. Dept. of the Interior, Geological Survey, 1985.
Знайти повний текст джерелаFolger, Peter F. Geochemical survey of the Baird Mountains 1p0sX3p0s quadrangle, Northwest Alaska. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1992.
Знайти повний текст джерелаTu Guangchi xue shu wen ji. Beijing: Ke xue chu ban she, 2010.
Знайти повний текст джерелаNash, J. Thomas. Geochemical signatures of ores and altered rocks in the Gilbert District, Esmeralda County, Nevada. [Reston, Va.?]: U.S. Dept. of the Interior, Geological Survey, 1985.
Знайти повний текст джерелаNash, J. Thomas. Geochemical signatures of ores and altered rocks in the Gilbert District, Esmeralda County, Nevada. [Reston, Va.?]: U.S. Dept. of the Interior, Geological Survey, 1985.
Знайти повний текст джерелаUnited States Geological Survey. Geochemical studies in Alaska by the U.S. Geological Survey, 1989. Denver, CO: U.S. Geological Survey, 1991.
Знайти повний текст джерелаFrisken, James G. Interpretation of reconnaissance geochemical data from the Port Moller, Stepovak Bay, and Simeonof Island quadrangles, Alaska peninsula, Alaska. Denver, CO: Dept. of the Interior, U.S. Geological Survey, 1992.
Знайти повний текст джерелаNash, J. Thomas. Geochemical signatures of ores and altered rocks in the Gilbert District, Esmeralda County, Nevada. [Reston, Va.?]: U.S. Dept. of the Interior, Geological Survey, 1985.
Знайти повний текст джерелаSheridan, Douglas M. Chemical data concerning Proterozoic ores and rocks from the Sedalia mine area, Chaffee County, Colorado. Denver, Colo: U.S. Dept. of the Interior, Geological Survey, 1988.
Знайти повний текст джерелаЧастини книг з теми "Ore geochemistry"
Barbieri, Mario. "Geochemistry of Barium." In Nonmetalliferous Stratabound Ore Fields, 9–15. Boston, MA: Springer US, 1989. http://dx.doi.org/10.1007/978-1-4684-6554-9_2.
Повний текст джерелаDahlkamp, Franz J. "Geochemistry and Minerochemistry of Uranium." In Uranium Ore Deposits, 17–39. Berlin, Heidelberg: Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-662-02892-6_3.
Повний текст джерелаUliana, Daniel, M. Manuela M. Lé Tassinari, Henrique Kahn, and Marco Antonio Angora. "Process Mineralogy of Lateritic Nickel Ore." In Springer Geochemistry/Mineralogy, 71–80. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_8.
Повний текст джерелаAzarnova, Liudmila. "Bolshetagninskoe Deposit Microcline–Pyrochlore Ore Process Mineralogy." In Springer Geochemistry/Mineralogy, 223–32. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_23.
Повний текст джерелаLecumberri-Sanchez, Pilar, and Robert J. Bodnar. "Halogen Geochemistry of Ore Deposits: Contributions Towards Understanding Sources and Processes." In Springer Geochemistry, 261–305. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-61667-4_5.
Повний текст джерелаWells, M. A., and E. R. Ramanaidou. "Raman Spectroscopic Core Scanning for Iron Ore and BIF Characterization." In Springer Geochemistry/Mineralogy, 387–96. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_39.
Повний текст джерелаHong, Qiuyang, Lili Zhang, and Bo Li. "The Occurrence of Sc, Co, and Ni in Lithiophorite-type Manganese Ore." In Springer Geochemistry/Mineralogy, 151–58. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_16.
Повний текст джерелаJones, D. G., and J. A. Plant. "Geochemistry of Shales." In Metallogenic models and exploration criteria for buried carbonate-hosted ore deposits—a multidisciplinary study in eastern England, 65–94. Boston, MA: Springer US, 1989. http://dx.doi.org/10.1007/978-1-4899-7184-5_6.
Повний текст джерелаÇiftçi, Emin, Abdurrahman Lermi, and Bülent Yalçınalp. "Ore Mineral Textures of Late Cretaceous Volcanogenic Massive Sulfide Deposits of Turkey: Proposed Paragenetic Sequence." In Springer Geochemistry/Mineralogy, 91–97. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_10.
Повний текст джерелаOhmoto, Hiroshi. "Chapter 14. STABLE ISOTOPE GEOCHEMISTRY of ORE DEPOSITS." In Stable Isotopes in High Temperature Geological Processes, edited by John W. Valley, Hugh P. Taylor, and James R. O’Neil, 491–560. Berlin, Boston: De Gruyter, 1986. http://dx.doi.org/10.1515/9781501508936-019.
Повний текст джерелаТези доповідей конференцій з теми "Ore geochemistry"
Maibam, B., S. F. Foley, and D. E. Jacob. "Geochemistry of Chromian Spinels from the Indo-Myanmar Ophiolite Belt of Northeastern India." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63395.
Повний текст джерелаManikyamba, C., and Abhishek Saha. "PGE Geochemistry of Komatiites from Neoarchean Sigegudda Greenstone Terrane, Western Dharwar Craton, India." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63398.
Повний текст джерелаMirza, Azimuddin. "GEOCHEMISTRY OF IRON ORE DEPOSITS FROM THE SINGHBHUM-ORISSA CRATON (INDIA)." In 15th International Multidisciplinary Scientific GeoConference SGEM2015. Stef92 Technology, 2011. http://dx.doi.org/10.5593/sgem2015/b13/s3.042.
Повний текст джерелаSatyanarayanan, M., S. P. Singh, D. S. Sarma, and V. Balaram. "Geochemistry of PGE-Bearing Ultramafic Rocks from Ikauna in Madawara Complex, Bundelkhand Craton, Central India." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63397.
Повний текст джерелаZamana, L. V., L. V. Taskina, and L. V. Zamana. "Geochemistry of Drainage Water of Darasun Ore Field Gold Deposits (Eastern Transbaikalia, Russia)." In Proceedings of the International Symposium "Engineering and Earth Sciences: Applied and Fundamental Research" dedicated to the 85th anniversary of H.I. Ibragimov (ISEES 2019). Paris, France: Atlantis Press, 2019. http://dx.doi.org/10.2991/isees-19.2019.130.
Повний текст джерелаFontaine, Joseph Edward, Samuel Fontaine, and G. Nelson Eby. "GEOCHEMISTRY OF ORE MINERALS AND CALCITE FROM THE FRANKLIN AND STERLING HILL ZINC MINES." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310671.
Повний текст джерелаSunder Raju, P. V., R. K. W. Merkle, R. H. Sawkar, and K. T. Vidyadharan. "Geology and Geochemistry of Ultramafic-Mafic Rocks from Antarghatta Belt, Western Dharwar Craton, Karnataka: Implications for PGE Mineralization and Future Targets." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63399.
Повний текст джерелаSubramanyam, K. S. V., V. Balaram, U. V. B. Reddy, Parijat Roy, and S. S. Sawant. "Trace, REE and PGE Geochemistry of the Mesoproterozoic Boggulakonda Gabbroic Rocks in the High-Grade Terrain Adjoining Nellore Schist Belt, South East India." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63400.
Повний текст джерелаUtevsky, Elinor S., John H. Dilles, Nansen H. Olson, and Adam J. R. Kent. "GEOCHEMISTRY OF CENOZOIC PLUTONIC ROCKS IN THE WESTERN CASCADES: TRACERS OF ARC EVOLUTION & ORE GENESIS." In 115th Annual GSA Cordilleran Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019cd-329847.
Повний текст джерелаPalma Lira, Gisella, Fernando Barra, Martin Reich, Adam Simon, and Rurik Romero Núñez. "Magmatic-hydrothermal ore-forming processes revealed by magnetite geochemistry of Chilean iron oxide-apatite (IOA) deposits." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.7122.
Повний текст джерелаЗвіти організацій з теми "Ore geochemistry"
Jonasson, I. R., E M Hillary, M. D. Hannington, P. Mercier-Langevin, and D. Diekrup. Trace-element geochemistry of ore-mineral separates from selected Canadian base-metal deposits. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2020. http://dx.doi.org/10.4095/326134.
Повний текст джерелаJonasson, I. R., D. E. Ames, and A. G. Galley. Sulphide ore geochemistry database for volcanogenic massive sulphide deposits of the Paleoproterozoic Flin Flon Belt and Sherridon area, Manitoba and Saskatchewan. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2009. http://dx.doi.org/10.4095/248125.
Повний текст джерелаLawley, C., B. Dubé, S. Jackson, Z. Yang, P. Mercier-Langevin, and D. Vaillancourt. Sulfide paragenesis and LA-ICP-MS arsenopyrite geochemistry at the Meliadine Gold District, Nunavut: implications for Re-Os arsenopyrite geochronology and ore deposit genesis. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2014. http://dx.doi.org/10.4095/293938.
Повний текст джерелаJamieson, H. E., and J. W. Lydon. Geochemistry of a fossil ore-solution aquifer: chemical exchange between rock and hydrothermal fluid recorded in the lower portion of research drill hole CY-2a, Agrokipia, Cyprus. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122592.
Повний текст джерелаKidder, J. A., M. B. McClenaghan, M I Leybourne, M. W. McCurdy, P. Pelchat, D. Layton-Matthews, C. E. Beckett-Brown, and A. Voinot. Geochemical data for stream and groundwaters around the Casino Cu-Au-Mo porphyry deposit, Yukon (NTS 115 J/10 and 115 J/15). Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328862.
Повний текст джерелаLane, L. S., K. M. Bell, and D. R. Issler. Overview of the age, evolution, and petroleum potential of the Eagle Plain Basin, Yukon. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/326092.
Повний текст джерелаJacques, I. J., A. J. Anderson, and S. G. Nielsen. The geochemistry of thallium and its isotopes in rare-element pegmatites. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328983.
Повний текст джерелаLacerda Silva, P., G. R. Chalmers, A. M. M. Bustin, and R. M. Bustin. Gas geochemistry and the origins of H2S in the Montney Formation. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329794.
Повний текст джерелаKuster, K., C. M. Lesher, and M. G. Houlé. Geology and geochemistry of mafic and ultramafic bodies in the Shebandowan mine area, Wawa-Abitibi terrane: implications for Ni-Cu-(PGE) and Cr-(PGE) mineralization, Ontario and Quebec. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329394.
Повний текст джерелаMcClenaghan, M. B., W. A. Spirito, S. J. A. Day, M. W. McCurdy, and R. J. McNeil. Overview of GEM surficial geochemistry and indicator mineral surveys and case studies in northern Canada. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330473.
Повний текст джерела