Tectonics and metallogeny of the junction zone between the North Asian craton and Pacific tectonic belt

详细信息    查看全文

• 作者：M. V. Goroshko ; B. F. Shevchenko ; V. A. Guryanov…
• 关键词：tectonics ; minerageny ; metallogenic zoning ; junction zone ; North Asian craton ; Pacific tectonic belt
• 刊名：Russian Journal of Pacific Geology
• 出版年：2016
• 出版时间：January 2016
• 年：2016
• 卷：10
• 期：1
• 页码：13-27
• 全文大小：573 KB
• 参考文献：1.A. D. Arkhangel’skii and N. S. Shatskii, “Tectonic scheme of the USSR,” Byull. Mosk. O-va Ispyt. Prir., Otd. Geol. 11 (4), 343 (1933).
  2.Yu. A. Bilibin, Metallogenic Provinces and Metallogenic Epochs (Izd.-vo AN SSSR, Moscow, 1961), Vol. 3 [in Russian].
  3.V. A. Buryak, V. Ya. Bespalov, V. N. Gagaev, B. A. Zarubin, and V. B. Troyan, New Geological–Economic Type of Zirconium Mineralization (Conditions of Formation and Prospects of Application) (Khabarovsk, 1999) [in Russian].
  4.N. P. Vasil’kovskii, Geological History of Northeastern Asia: Siberian Platform and Verkhoyansk–Chukotka Region (Nauka, Moscow, 1981) [in Russian].
  5.Yu. A. Vashchilov, “Deep-seated faults of the Yana–Kolyma Fold Zone of the Okhotsk–Chukotka Volcanic Belt and their role in the formation of granitoid intrusions and structures,” Sov. Geologiya, No. 4, 54–72 (1963).
  6.G. N. Gamyanin, V. I. Goncharov, and N. A. Goryachev, “Gold–rare-metal deposits of Northeast Russia,” Tikhookean. Geol., No. 3, 94–103 (1998).
  7.Geodynamics, Magmatism, and Metallogeny of East Russia, Ed. by A. I. Khanchuk (Dal’nauka, Vladivostok, 2006) [in Russian].
  8. Geological Map of Northeast USSR. 1: 1500000 (Leningrad, 1980) [in Russian].
  9. Geology of Gold Deposits of the East USSR (TsNIGRI, Moscow, 1988), p. 264 [in Russian].
  10. Geology of the USSR. Volume 30. Part. 1. Book. 2. Mineral Resources, Ed. by A. V. Sidorenko (Nedra, Moscow, 1970) [in Russian].
  11. Geology of the USSR. Volume 30. Part 2. Mineral Resources, Froundwaters, (Nedra, Moscow, 1983) [in Russian].
  12.M. V. Goroshko and V. E. Kirillov, “New data on the absolute age of rare-metal mineralization in the southeastern part of the Aldan Shield,” in Proceedings of Association of Geological Organizations of the Far East (Dal’nedra, Khabarovsk, 1992), No. 2, pp. 66–69 [in Russian].
  13.M. V. Goroshko and V. A. Gur’yanov, “Uranium–rare metal mineralization in the ultrabasic alkaline massifs of the southeastern Siberian Platform,” Tikhookean. Geol. 20 (6), 76–91 (2004).
  14.M. V. Goroshko, Yu. F. Malyshev, and V. E. Kirillov, Uranium Metallogeny of the Russian Far East (Nauka, Moscow, 2006) [in Russian].
  15.M. V. Goroshko and V. A. Gur’yanov, “Ore mineralization related to the zone of the pre-Riphean structural stratigraphic unconformity and Lower Riphean platformal cover of the Uchur–Maya Depression, the southeastern Siberian Platform,” Russ. J. Pac. Geol. 1 (6), 586–601 (2007).CrossRef
  16.M. V. Goroshko, V. A. Gur’yanov, N. V. Berdnikov, and V. E. Kirillov, “Gold potential of the volcanoplutonic zones in the southeastern Siberian Platform and physicochemical conditions of the deposit formation,” Russ. J. Pac. Geol. 3 (6), 511–529 (2009).CrossRef
  17.M. V. Goroshko and G. Z. Gil’manova, “Lithological and structural prerequisites for localization of ore deposits in the Mesoproterozoic–Neoproterozoic Uchur–Maya Depression (Siberian Platform),” Russ. J. Pac. Geol. 7 (4), 262–276 (2013).CrossRef
  18.N. A. Goryachev, V. I. Gvozdev, and A. S. Vakh, “Metallogeny of the Russian Far East,” in Geological Processes in Subduction, Collisional, and Transform-Plate Margin Settings. Proceedings of 2nd All-Russian Conference with International Participation, Vladivostok, Russia, 2014 (Dal’nauka DVO RAN, Vladivostok, 2014), pp. 310–311 [in Russian].
  19.V. A. Gur’yanov, Geology and Metallogeny of the Ulkan Region (Aldan-Stanovoi Shield) (Dal’nauka, Vladivostok, 2007) [in Russian].
  20.V. A. Gur’yanov, V. S. Prikhod’ko, A. N. Perestoronin, L. L. Petukhova, A. Yu. Peskov, and A. V. Kosynkin, “Platinum potential of Ni-bearing mafic–ultramafic rocks of the Pristanovoi collisional belt,” in Proceedings of All-Russian Conference. 8th Kosygin Readings: “Tectonics, Deep Structure, and Metallogeny”, Vladivostok, Russia, 2013 (Dal’nauka, Vladivostok, 2013), pp. 242–246 [in Russian].
  21.V. A. Gur’yanov, A. N. Perestoronin, A. N. Didenko, A. Yu. Peskov, A. V. Kosynkin, “Late Paleoproterozoic basic dikes in the Ulkan–Uchur District, eastern Aldan–Stanovoi Shield: structural position, composition, and paleogeodynamic setting,” Geotectonics 47 (4), 279–290 (2013).CrossRef
  22.A. N. Didenko, V. A. Gur’yanov, A. Yu. Peskov, A. N. Perestoronin, D. V. Avdeev, E. V. Bibikova, T. I. Kirnozova, and M. M. Fugzan, “Geochemistry and geochronology of the Proterozoic magmatic rocks of the Ulkan Trough: new data,” Russ. J. Pac. Geol. 4 (5), 398–417 (2010).CrossRef
  23.A. N. Didenko, A. Yu. Peskov, V. A. Gur’yanov, A. N. Perestoronin, and A. V. Kosynkin, “Paleomagnetism of the Ulkan Trough (southeastern Siberian Craton),” Russ. J. Pac. Geol. 7 (1), 26–45 (2013).CrossRef
  24.L. P. Karsakov, V. A. Gur’yanov, and M. V. Goroshko, “Stratigraphy of lower horizons in the Siberian hypostratotype of the Riphean (the southeastern Siberian Platform),” Stratigr. Geol. Correlation, 10 (1), 42–56 (2002).
  25.V. E. Kirillov and M. V. Goroshko, “Uranium metallogeny of the Ul’in and Kuidusun volcanogenic troughs,” Tikhookean. Geol., No. 3, 88–97 (1996).
  26.S. G. Kislyakov, “Magmatic complexes of the central southern Verkhoyansk region,” in Proceedings of the Dal’nedra Association, (Dal’nedra, Khabarovsk, 1992), No. 2, pp. 32–36 [in Russian].
  27.I. N. Kotlyar, Au–Ag Ore Potential of the Okhotsk–Chukotka Belt (Nauka, Moscow, 1986) [in Russian].
  28.P. N. Kropotkin and N. P. Kheraskov, “Tectonics of Northeastern Russia,” in International Geological Congress. Proceedings of 27th Session (GONTI, Moscow, 1937), Vol. 2, p. 207 [in Russian].
  29.E. P. Mironyuk, Geological Map of the USSR. 1: 1000000 (New Series). Sheet O-(52), 53-Tommot: Explanatory Notes (Leningrad, 1986) [in Russian].
  30.S. V. Obruchev, “Tectonics of northeastern Asian,” in Proceedings of 17th Session of the International Geological Congress, 1937, (GONTI, Moscow, 1940), Vol. 5, pp. 211–218 [in Russian].
  31.L. M. Parfenov, U. J. Nokleberg, J. U. Monger, et al., “Formation of the terrane collage of the orogenic belts in the northern Pacific margin,” Geol. Geofiz. 40 (11), 1563–1574 (1999).
  32.V. F. Polin, V. G. Sakhno, G. P. Sandimirova, and L. S. Tsurikova, “Petrology of Mesozoic monzonite–syenite magmatism of the Ketkap–Yuna magmatic province in the Aldan Shield,” Dokl. Earth Sci. 418 (1), 9–14 (2008).CrossRef
  33.Yu. M. Pushcharovskii, Doctoral Dissertation in Geology and Mineralogy (Moscow, 1958).
  34.Yu. M. Pushcharovskii, Marginal Troughs, Their Tectonic Structure, and Evolution (Moscow, 1959) [in Russian].
  35.A. M. Semikhatov and S. N. Serebryakov, Sibirskii gipostratotip rifeya (Nedra, Moscow, 1983) [in Russian].
  36.N. V. Sitnikov, V. E. Kirillov, and V. S. Alekseev, “Molybdenum mineralization of the eastern Okhotsk Massif,” Tikhookean. Geol., No. 4, 73–77 (1991).
  37.A. L. Stavtsev, Tectonics and Mineral Resources of the Junction Zones between Ancient Platforms and Mobile Belts (Nedra, Moscow, 1983) [in Russian].
  38.A. L. Stavtsev, State Geological Map of the USSR. 1: 1000000 (New Series). Sheet O -(53), -54—Okhotsk: Explanatory Notes (Leningrad, 1988) [in Russian].
  39.G. A. Stognii and V. V. Stognii, Geophysical Fields of the Eastern North Asian Craton (Sakhapoligrafizdat, Yakutsk, 2005) [in Russian].
  40. Tectonic Map of the USSR. 1: 4000000, Ed. by N.S. Shatsky (Omsk, 1953) [in Russian].
  41.Tectonics, Geodynamics, and Metallogeny of the Sakha Republic Territory (Yakutia), Ed. by L. M. Parfenov and M. I. Kuz’min (Nauka/Interperiodika, Moscow, 2001) [in Russian].
  42. Tectonics, Deep Structure, and Metallogeny of the Junction Zone of the Central Asian and Pacific Belts: Explanatory Notes to the Tectonic Map—1: 1500000, Ed. by L. P. Karsakov, Chzhao Chun’tszin, Yu. F. Malyshev, M. V. Goroshko, et al., (Vladivostok–Khabarovsk, 2005) [in Russian].
  43. Tectonics of the Continental Margins of Northwestern Pacific Ocean, Ed. by M. S. Markov, Yu. A. Pushcharovsky, S. M. Til’man et al., (Nauka, Moscow, 1980) [in Russian].
  44. Tectonic Map of North Eurasia. 1: 5000000, Ed. by A. V. Peive and L. A. Yanshin (GUGK, Leningrad, 1980) [in Russian].
  45. Tectonic Map of the USSR and Adjacent Countries. 1: 5000000, Ed. by N. S. Shatsky (Gosgeoltekhizdat, Moscow, 1956) [in Russian].
  46.S. M. Til’man, S. G. Byalobzheskii, A. D. Chekhov, and L. L. Krasnyi, “Features of the formation of continental crust in the northeast USSR,” Geotektonika, No. 6, 15–29 (1975).
  47.A. D. Chekhov, Tectonic Evolution of Northeast Asia (Nauch. mir, Moscow, 2000) [in Russian].
  48.A. A. Schneider, Yu. F. Malyshev, M. V. Goroshko, and N. P. Romanovskii, “Complex mineralization at large ore deposits in the Russian Far East,” Geol. Ore Deposits 53 (2), 140–155 (2011).CrossRef
  49.E. V. Yalynychev and G. S. Mirzekhanov, “Gold–base metal mineralization in the sedimentary cover of the southeastern Siberian Platform (Uchur District),” in Mineralogy of the Far East Deposits (Vladivostok, 1988), pp. 71–80 [in Russian].
  
• 作者单位：M. V. Goroshko (1)
  B. F. Shevchenko (1)
  V. A. Guryanov (1)
  G. Z. Gil’manova (1)
  
  1. Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences, ul. Kim Yu Chena 65, Khabarovsk, 680000, Russia
  
• 刊物主题：Geology;
• 出版者：Springer US
• ISSN：1819-7159

文摘

The tectonics and metallogeny of the junction zone between the North Asian craton and Pacific tectonic belt are considered. This zone is characterized by a wide variety of structures superposed on the metamorphic basement, which was formed in the course of a multistage geologic development of the craton from the Precambrian to the Cenozoic. They are related to the craton evolution and its response to the collision and subduction processes in the adjacent orogenic belt, processes in the passive and active continental margins, and plume magmatism. The geological structure of the region includes blocks of metamorphic rocks of the Aldan–Stanovoi shield, Paleoproterozoic volcanogenic troughs, Mesoproterozoic–Neoproterozoic and Early Paleozoic structures of the platform cover, Late Paleozoic volcanic and terrigenous troughs, structures of the Late Mesozoic Okhotsk–Chukotka volcanic belt of the active continental margin, and Late Cretaceous riftogenic structures formed in response to plume magmatism. In total, six metallogenic epochs are recognized in the development of ore mineralization: Archean–Early Paleoproterozoic, Late Paleoproterozoic, Mesoproterozoic, Neoproterozoic, Late Paleozoic, and Late Mesozoic. The minerageny of the junction zone between the craton and Pacific belt is highly diversified, being characterized by distinct evolution in time and space. Each development stage features its own set of mineral resources.