Peer-reviewed articles 17,970 +



Title: RARE-EARTH MINERALIZATION IN GRANITES OF THE NORTH-EAST OF THE VERKHOYANSK-KOLYMA OROGEN

RARE-EARTH MINERALIZATION IN GRANITES OF THE NORTH-EAST OF THE VERKHOYANSK-KOLYMA OROGEN
Vera Trunilina
10.5593/sgem2023/1.1
1314-2704
English
23
1
•    Prof. DSc. Oleksandr Trofymchuk, UKRAINE 
•    Prof. Dr. hab. oec. Baiba Rivza, LATVIA
The results of the study of granites of the north-east of the Verkhoyansk-Kolyma orogen bearing rare-earth mineralization are summarized in the article. Ore-bearing granites are classified as A-type of postorogenic and rift-related geodynamic conditions. Three groups are identified in them, differing in the origin and scale of the associated rareearth mineralization. The most ore-bearing granites are spatially and genetically related to alkaline–ultrabasic – alkaline-basic formations and formed within a long-lived hotspot from granite melt, generated from a fenitized crustal substrate under the influence of a flow of transmagmatic fluids. Granite massifs are limited ore-bearing, crystallized from melts generated in the Paleoproterozoic substrates of the lower crust under the influence of heat and fluids, related to the mantle magmas and bearing clear signs of mixing of basic and acidic melts during crystallization. These massifs are localized within the Indigirka crustal extension belt, where the presence of buried centers of the basic melts is assumed, which activation caused the re-melting of crustal substrates. Granites that do not bear signs of mantle-crustal interaction usually have only dispersed accessory rare-earth mineralization.
[1] Mikhailov V.A. Rare-earth ores of the world. Kiev, Ukraine, Publishing House "Kiev University", 2010, 223 pp.
[2] Trunilina V.A. Late cretaceous granites of the Selennyakh Ridge (Verkhoyansk- Kolyma Orogenic Area). Solid State Technology, USA, vol. 63, Issue: 3, 2020, pp. 4501–4525.
[3] Trunilina V.A., Prokopiev A.V. Petrology of Granites of the Tommot Rare-Earth Ore Field (Verkhoyansk–Kolyma Orogenic Belt). Minerals, Switzerland, № 12(11), 2022, 33 pp.
[4] Parfenov L.M., Kuzmin M.I. (Eds.) Tectonics, Geodynamics and Metallogeny of the Territory of the Republic of Sakha (Yakutia). Moscow, Russia: MAIK Nauka/Interperiodika: 2001; 571 pp.
[5] Jung S., Pfander J.A. Source composition and melting temperatures of orogenic granitoids – constrains from CaO/Na2O, Al2O3/TiO2 and accessory mineral saturation thermometry. European Journal of Mineralogy, Germany, № 1, 2007, pp. 5–40.
[6] Maniar P.D., Piccoli, P.M. Tectonic discrimination of granitoids. Geological Society of America Bulletin, USA, vol. 101, 1989, pp. 635–643.
[7] Maeda J. Opening of the Kuril Basin deduced from the magmatic history of Central Hokkaido northern Japan. Tectonophysics, Netherlands, vol. 174, 1990, pp. 235–255.
[8] Datsenko V.М. Petrogeochemical typification of granitoids of the south-western framing of the Siberian platform. Materials of the Second All-Russian Petrographic Meeting: Syktyvkar, Russia, vol. 2, 2000, pp. 270–274.
[9] Pearce J.A., Harris N.B.W., Tindle A.G. Trace element discrimination diagrams for the tectonic interpretation of the granitic rocks. Petrology, Germany, vol. 25, pt. 44, 1984, pp. 956–963.
[10] Eby G.N. Chemical subdiwision of the A-type granitouids: petrogenetic and tectonic implications. Geology, Germany, № 20, 1992, pp. 641–644.
[11] Grebennikov A.V. Granitoids of type A: problems of diagnosis, formation and systematics. Geology and Geophysics, Russia, vol. 55 (9), 2014, pp.1356-1373.
[12] Belyaev G.M., Rudnik, V.A. Formation and genetic types of granitoids. Ltningrad: Nedra, Russia, 1978, 168 pp.
[13] Janousek V., Farrow C. M., Erban V. Interpretation of whole-rock geochemical data in igneous geochemistry: introducing Geochemical Data Toolkit (GCDkit). Petrology, Germany, vol. 47, 2006, pp. 1255–1259.
[14] King P.L., White A.J.R., Chappell B.W., Allen C.M. Characterization and Origin of aluminous A-type Granites from the Lachlan Fold Belt, Southeastern Australia. Petrology, Germany, vol. 38, 1997, pp. 371–391.
[15] Martin R.F. A-Type Granites of Crustal Origin Ultimately Result from Open- System Fenitization-Type Reactions in an Extensional Environment. Lithos, Netherlands, vol. 91, 2006, pp.125–136.
[16] Sazonova, L.V., Nosova А.А., Dokuchaev А.Y., Gurbanov А.G. Latite type of late collisional granitoids (North Caucasus): geochemical and mineralogical features. RAS report, Russia, vol. 393, № 2, 2003, pp. 2–5.
[17] Whalen J. A-type granites in New Brunswick. Geological Survey Canada Paper, Canada, N 1a, 1986, P. 297–300.
[18] Kashubin O. V., Petrov S. P., Shokalsky E. D. The deep structure of the Earth's crust of Northeastern Eurasia and its continental margins. Geodynamics and Tectonophysics, Russia, vol. 12, № 2, 2021, pp. 199–224.
[19] Yarmolyuk V.V., Nikiforov A.V., Kozlovsky A.M., Kudryashova E.A. Late Mesozoic magmatic province of East Asia: structure, magmatism and conditions of formation. Geotectonics, Russia, № 4, 2019, pp. 60–77.
conference
Proceedings of 23rd International Multidisciplinary Scientific GeoConference SGEM 2023
23rd International Multidisciplinary Scientific GeoConference SGEM 2023, 03 - 09 July, 2023
Proceedings Paper
STEF92 Technology
International Multidisciplinary Scientific GeoConference-SGEM
SWS Scholarly Society; Acad Sci Czech Republ; Latvian Acad Sci; Polish Acad Sci; Russian Acad Sci; Serbian Acad Sci and Arts; Natl Acad Sci Ukraine; Natl Acad Sci Armenia; Sci Council Japan; European Acad Sci, Arts and Letters; Acad Fine Arts Zagreb Croatia; Croatian Acad Sci and Arts; Acad Sci Moldova; Montenegrin Acad Sci and Arts; Georgian Acad Sci; Acad Fine Arts and Design Bratislava; Russian Acad Arts; Turkish Acad Sci.
133-146
03 - 09 July, 2023
website
9006
granites, ore content, rare-earth minerals, mantle-crustal interaction

24th SGEM International Conference on Earth & Planetary Sciences


International GeoConference SGEM2024
28 June - 8 July, 2024 / Albena, Bulgaria

Read More
   

SGEM Vienna GREEN "Green Science for Green Life"


Extended Scientific Sessions SGEM Vienna GREEN
25 - 29 November, 2024 / Vienna, Austria

Read More
   

A scientific platform for Art-Inspired Scientists!


The Magical World Where Science meets Art
Vienna, Austria

Read More