 | Sotnikov, V.I., Sorokin, A.A., Ponomarchuk, V.A., Gimon, V.O., Sorokin, A.P. (2007) Porphyry Cu-Mo-(Au) mineralization: the age and relationship with igneous rock complexes of the Borgulikan ore field (upper-Amur region) Russian Geology and Geophysics, 48 (2) 177-184 doi:10.1016/j.rgg.2007.02.003 | Journal (article/letter/editorial) | | with igneous rock complexes of the Borgulikan ore field (upper-Amur region) V.I. Sotnikov a, A.A. Sorokin... 3 prosp. Akad. Koptyuga, Novosibirsk, 630090, Russia Institute of Geology and Nature Management, Far...Blagoveshchensk, 675000, Russia Received 14 June 2005 Abstract The Borgulikan ore field is localized in the...volcanoplutonic belt made up of various igneous (upper-Amur granite-granodiorite (140–134 Ma), Burunda monz...mineralization yielded the following ages: early (dark) “pre-ore” quartz monzodiorite porphyrites — 125.8±0.7 Ma (groundmass) |  | Buchko, I. V., Buchko, Ir. V., Sorokin, A. A., Ponomarchuk, V. A., Travin, A. V. (2014) Localization of mineralization, its age, and relationship to magmatism at the Mogot silver-base-metal deposit, North Stanovoi metallogenic zone in the southeastern framework of the North Asian Craton. Geology of Ore Deposits, 56 (2) 101-112 doi:10.1134/s1075701514020020 | Journal (article/letter/editorial) | | ISSN 10757015, Geology of Ore Deposits, 2014, Vol. 56, No. 2, pp. 101–112. © Pleiades Publishing, Ltd...ul. B. Khmel’nitskogo 2, Blagoveshchensk, 675000 Russia b Institute of Geology and Mineralogy, Siberian...prosp. Akademika Koptyuga 3, Novosibirsk, 630090 Russia Received July 1, 2013 Abstract—The results of...Superterrane are discussed in this paper. The main orecontrolling structural elements of the studied district...total sulfide content in ore is 2–3%. The high Ag, Pb, and Zn contents in ore allow us to consider the |  | Kadashnikova, A. Yu., Sorokin, A. A., Ponomarchuk, V. A., Travin, A. V., Ponomarchuk, A. V., Eirish, L. V. (2019) Distribution of Mineralization, Ages, and Sources of the Malomyr Gold Deposit, Eastern Part of the Mongol–Okhotsk Fold Belt. Geology of Ore Deposits, 61 (1) 1-13 doi:10.1134/s1075701519010045 | Journal (article/letter/editorial) | | ISSN 1075-7015, Geology of Ore Deposits, 2019, Vol. 61, No. 1, pp. 1–13. © Pleiades Publishing, Ltd....Russian Academy of Sciences, Blagoveshchensk, 675000 Russia b Institute of Geology and Mineralogy, Siberian...Russian Academy of Sciences, Novosibirsk, 630090 Russia *e-mail: askad7497@mail.ru Received May 14, 2018;...obtained data indicate that the age of the hydrothermal ore process that led to the formation of the Malomyr...region 134–130 Ma ago, making impossible to link the ore mineralization of the Malomyr deposit to magmatic |  | | Journal (article/letter/editorial) | | flank of the Umlekan–Ogodzha volcanoplutonic belt (Amur region) A.A. Sorokin a,*, A.P. Sorokin a, V.A. Ponomarchuk...Sciences, 1 per. Relochnyi, Blagoveshchensk, 675000, Russia V.S. Sobolev Institute of Geology and Mineralogy... 3 prosp. Akad. Koptyuga, Novosibirsk, 630090, Russia Received 22 December 2008; received in revised...the W–E direction along the boundary between the Amur superterrane and the eastern Mongolo–Okhotsk fold...serpentine, and accessory minerals are apatite and magnetite. Andesites are dark gray, black, and dark green |  | Asadi, Hooshang H., Porwal, Alok, Fatehi, Moslem, Kianpouryan, Sadegh, Lu, Yong-Jun (2015) Exploration feature selection applied to hybrid data integration modeling: Targeting copper-gold potential in central Iran. Ore Geology Reviews, 71. 819-838 doi:10.1016/j.oregeorev.2014.12.001 | Journal (article/letter/editorial) | | oregeorev.2014.12.001 OREGEO 1395 To appear in: Ore Geology Reviews Received date: Revised date: Accepted...targeting copper-gold potential in central Iran, Ore Geology Reviews (2014), doi: 10.1016/j.oregeorev...targeting requires (a) a clear understanding of ore-forming processes and relevant recognition criteria...characterized by intense potassic alteration (quartz, magnetite, secondary biotite and K-feldspar) associated...mineralization mainly occurs in the NU quartz-magnetite stockworks, veins and veinlets (Fig. 3). Hypogene |
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