Abstract
The geochemical features of typical representatives of ferromanganese deposits are studied in the eastern Bureya and Khanka massifs (Russian Far East). Based on the major-, trace-, and rare-earth element distribution, the hydrothermal–sedimentary (with hydrogenic component) nature of their mineralization is established and the geodynamic setting and depth of ore formation are estimated. The differences in the depth and redox conditions of ore formation resulted in the metallogenic zonation of the Khingan block (Bureya Massif), which is expressed in a westward change in ore composition from the magnetite ores of the Kosten’ga–Kimkan zone to the hematite–magnetite and iron–manganese ores of the South Khingan zone. The conclusions about the participation of hydrothermal sources in the formation of ore mineralization of the studied deposits and the specifics of their localization require revision of the strategy of exploration and evaluation of ferromanganese ores in the southern Far East.
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References
E. S. Bazilevskaya, Study of Ferromanganese Ores of the Ocean (Nauka, Moscow, 2007) [in Russian].
I. M. Varentsov, V. A. Drits, A. I. Gorshkov, and Yu. K. Andreev, “Formation of Fe–Mn crusts in the Atlantic: mineralogy, geochemistry of major and trace elements, Krylov seamount,” in Genesis of Sediments and Fundamemtal Problems of Lithology (Nauka, Moscow, 1989), pp. 58–78 [in Russian].
Guyots of Western Pacific and Their Ore Potential, Ed. by Yu. G. Volokhin, M. E. Mel’nikov, E. L. Shkol’nik et al., (Nauka, Moscow, 1995) [in Russian].
Geodynamics, Magmatism, and Metallogeny of East Russia, Ed. by A. I. Khanchuk (Dal’nauka, Vladivostok, 2006) [in Russian].
Geology of USSR. Vol. 19. Khabarovsk Krai and Amur Oblast. Part 1. Geological Description, Ed. by L. I. Krasnyi (Nedra, Moscow, 1966) [in Russian].
State Geological Map of the Russian Federation. 1: 1000000 (Third Generation). Far East Series. Sheet L-(52), 53; (K-52, 53) Lake Khanka. http://wwwgeokniga. org/maps/7156
State Geological Map of the Russian Federation. 1: 1000000 (Third Generation). Far East Series. Sheet M-52—Blagoveshchensk. http://wwwgeoknigaorg/ maps/7417
E. G. Gurvich, Metalliferous Sediments of the World Ocean (Nauch. mir, Moscow, 1998) [in Russian].
A. V. Dubinin, T. Yu. Uspenskaya, G. M. Gavrilenko, and V. A. Rashidov, “Geochemistry and genesis of Fe–Mn mineralization in island arcs in the west Pacific Ocean,” Geochem. Int. 46 (12), 1206–1227 (2008).
E. V. Egorov and M. V. Timofeeva, “Effusive ferrosiliceous formations and iron ore deposits of Lesser Khingan,” in Geology and Genesis of of the Precambrian Ferrosiliceous and Manganese Formations around the World. Proceedings of International Symposium (Nauk. Dumka, Kiev, 1972), pp. 188–195 [in Russian].
V. V. Zaikov and I. Yu. Melekestseva, “Cobalt–copper sulfide deposits in the ultramafites of accretionary wedge of the Western Magnitogorsk paleoisland arc,” Litosfera, No. 3, 73–98 (2005).
Rich Cobalt Ores of the World Ocean (VNIIOkeangeologiya, St. Petersburg, 2002) [in Russian].
A. B. Kotov, S. D. Velikoslavinskii, A. A. Sorokin, L. N. Kotova, A. P. Sorokin, A. M. Larin, V. P. Kovach, N. Yu. Zagornaya, and A. A. Kurguzova, “Age of the Amur Group of the Bureya–Jiamusi Superterrane in the Central Asian Fold Belt: Sm-Nd isotope evidence,” Dokl. Earth Sci. 429 (8), 1245–1248 (2009).
E. A. Kulish, L. I. Kulish, K. M. Merkur’ev, and E. A. Panskikh, Manganese–Banded Iron Formation of the USSR Far East (Nauka, Moscow, 1981) [in Russian].
Metallogeny of Series of the Island Arc Geodynamic Settings, Ed. by N. V. Mezhelovskii (IMGRE, Moscow, 1999) [in Russian].
P. E. Mikhailik, E. V. Mikhailik, N. V. Zarubina, N. N. Barinov, V. T. S”edin, and E. P. Lelikov, “Composition and distribution of REE in ferromanganese crusts of the Belyaevsky and Medvedev seamounts in the Sea of Japan,” Russ. J. Pac. Geol. 8 (5), 315–329 (2014).
V. G. Nevstruev, “Estimation of facies conditions of sedimentation of the ancient metalliferous sediments using iron–manganese ratios,” in Tectonics, Deep Structure, and Metallogeny of East Asia: 8th Kosygin Readings. Proceedings of the All-Russian Conference, Khabarovsk, Russia, 2013 (Dal’nauka, Vladivostok, 2013), pp. 302–306 [in Russian].
V. G. Nevstruev, B. G. Saksin, V. I. Usikov, and N. V. Berdnikov, Cryptovolcanic ancient rocks of the Lesser Khingan,” in Geological Processes in Subduction, Collision, and Lithospheric Plate Sliding Settings. Proceedings of the 2nd All-Russian Conference with International Participation, Vladivostok, Russia, 2014 (Dal’nauka, Vladivostok, 2014), pp. 213–216 [in Russian].
V. G. Nevstruev, N. V. Berdnikov, B. G. Saksin, and V. I. Usikov, “Noble metal mineralization in the carbonaceous rocks of the Poperechnoe iron–manganese deposit (Lesser Khingan, Russia),” Tikhookean. Geol. 9 (6), 102–111 (2015).
L. M. Parfenov, N. A. Berzin, A. I. Khanchuk, G. Badarch, V. G. Belichenko, A. N. Bulgatov, S. I. Dril’, G. L. Kirillova, M. I. Kuz’min, U. J. Nokleberg, A. V. Prokop’ev, V. F. Timofeev, O. Tomurtogoo, and H. Yan, “Genetic model of orogenic belts of Central and Northeastern Asia,” Tikhookean. Geol. 22 (6), 7–41 (2003).
A. A. Sorokin, A. B. Kotov, E. B. Sal’nikova, A. P. Sorokin, S. Z. Yakovleva, A. M. Fedoseenko, and Yu. V. Plotkina, “First data on the age of Early Paleozoic granitoids from the Malyi Khingan terrane of the Central Asian Fold Belt,” Dokl. Earth Sci. 431 (1), 299–303 (2010).
Khain, V. E. and Lomize, M.G., Geotectonics with Fundamentals of Geodynamics (Mosk. Gos. Univ., Moscow, 1995).
A. I. Khanchuk, “Tectonics and magmatism of the Californian-type paleotransform continental margins on Russian East,” in General Problems of Tecctonics. Tectonics of Russia. Proceedings of the 23rd Tectonic Conference (GEOS, Moscow, 2000), pp. 544–547 [in Russian].
A. I. Khanchuk, V. P. Molchanov, E. I. Medvedev, and L. P. Plyusnina, “Genetic types of gold-ore mineralization in graphite-bearing rocks of the southern Far East,” Dokl. Earth Sci., 430 (1), 86–89 (2010).
A. I. Khanchuk, V. P. Nechaev, L. P. Plyusnina, N. V. Berdnikov, V. P. Molchanov, and S. V. Vysotskii, “Noble metals in graphite-bearing rocks (a new type),” in Metallgenic Problems of Russia (GTs RAN, Moscow, 2012), pp. 287–301 [in Russian].
A. I. Khanchuk, V. G. Nevstruev, N. Berdnikov, and V. P. Nechaev, “Petrochemical characteristics of carbonaceous shales in the eastern Bureya Massif and their precious-metal mineralization,” Russ. Geol. Geophys. 54 (6), 627–636 (2013).
M. V. Chebotarev, “Geological structure of the South Khingan manganese deposit and composition of its ores,” Sov. Geol., No. 8, 114–136 (1958).
M. Bau and P. Dulski, “Comparative study of yttrium and rare-earth elements behaviors in fluorine-rich hydrothermal fluids,” Contrib. Mineral. Petrol. 119, 213–223 (1995).
M. Bau, K. Schmidt, A. Koschinsky, J. Hein, T. Kuhn, and A. Usui, “Discriminating between different genetic types of marine ferro-manganese crusts and nodules based on rare earth elements and yttrium,” Chem. Geol. 381, 1–9 (2014).
C. E. Fitzgerald and K. M. Gillis, “Hydrothermal manganese oxide deposits from Baby Bare Seamount in the northeast Pacific Ocean,” Mar. Geol. 225, 145–156 (2006).
E. R. Force and W. F. Cannon, “Depositional model for shallow-marine manganese deposits around black shale basins,” Econ. Geol. 83, 93–117 (1988).
F. Franchia, A. Hofmann, B. Cavalazzic, A. Wilson, and R. Barbieri, “Differentiating marine vs hydrothermal processes in Devonian carbonate mounds using rare earth elements (Kess Kess mounds, Anti-Atlas, Morocco),” Chem. Geol. 409, 69–86 (2015).
J. R. Hein, M. G. Stamatakis, and J. S. Dowling, “Trace metal-rich Quaternary hydrothermal manganese oxide and barite deposit, Milos Island, Greece,” Trans. Inst. Mining Metall. Sec. B, Appl. Earth Sci. 109, 67–76 (2000).
J. R. Hein, M. S. Schulz, R. E. Dunham, R. J. Stern, and S. H. Bloomer, “Diffuse flow hydrothermal manganese mineralization along the active Mariana and southern Izu-Bonin arc system, western Pacific,” J. Geophys. Res. 113, 14 (2008).
R. A. Mills and D. V. Wells, “Genesis of ferromanganese crust from the TAG hydrothermal field,” Chem. Geol. 176, 283–293 (2001).
S. M. McLennan, “Relationships between the trace composition of sedimentary rocks and upper continental crust,” Geochem., Geophys., Geosyst., 24, 2001. http:// onlinelibrarywileycom/doi/10.109/2000GC000109/pdf
R. W. Murray, “Chemical criteria to identify the depositional environment of chert: general principles and applications,” Sediment. Geol. 90, 213–232 (1994).
T. Plank and C. H. Langmuir, “The chemical composition of subducting sediment and its consequences for the crust and mantle,” Chem. Geol. 145 (3–4), 325–394 (1998).
D. Schissel and P. Aro, “The major Early Proterozoic sedimentary iron and manganese deposits and their tectonic setting,” Econ. Geol. 87, 1367–1374 (1992).
N. Tribovillard, E. Hatem, O. Averbuch, F. Barbecot, V. Bout-Roumazeilles, and A. Trentesaux, “Iron availability as a dominant control on the primary composition and diagenetic overprint of organic-matter-rich rocks,” Chem. Geol. 401, 67–82 (2015).
A. Usui, M. Bau, and T. Yamazaki, “Manganese mucrochimneys buried in the central Pacific pelagic sediments: evidence of intraplate water circulation?,” Mar. Geol. 141, 269–289 (1997).
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Original Russian Text © N.V. Berdnikov, V.G. Nevstruev, B.G. Saksin, 2016, published in Tikhookeanskaya Geologiya, 2016, Vol. 35, No. 4, pp. 28–39.
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Berdnikov, N.V., Nevstruev, V.G. & Saksin, B.G. Sources and formation conditions of ferromanganese mineralization of the Bureya and Khanka massifs, Russian Far East. Russ. J. of Pac. Geol. 10, 263–273 (2016). https://doi.org/10.1134/S1819714016040023
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DOI: https://doi.org/10.1134/S1819714016040023