Khodorevskaya, L. I. (2012). Granulite facies metamorphism and metasomatism in the gabbro-anorthosites of the Kolvitsa massif, Kola Peninsula. Geochemistry International, 50(3), 272-288.

Serov, P.A. (2020) The Paleoproterozoic Kandalaksha-Kolvitsa Gabbro-Anorthosite Complex (Fennoscandian Shield): New U–Pb, Sm–Nd, and Nd–Sr (ID-TIMS) Isotope Data on the Age of Formation, Metamorphism, and Geochemical Features of Zircon (LA-ICP-MS). Minerals 10, 254.

Reference Search (possible matching items)

	Steshenko, E. N., Nikolaev, A. I., Bayanova, T. B., Drogobuzhskaya, S. V., Chashchin, V. V., Serov, P. A., Lyalina, L. M., Novikov, A. I., Elizarov, D. V. (2018) The Paleoproterozoic Kolvitsa Anorthosite Massif: New Data on the U–Pb Age (ID TIMS) and Geochemical Features of Zircon. Doklady Earth Sciences, 479 (1) 366-370 doi:10.1134/s1028334x18030224	Journal (article/letter/editorial)
	GEOCHEMISTRY The Paleoproterozoic Kolvitsa Anorthosite Massif: New Data on the U–Pb Age (ID TIMS) and...2015 Abstract—The rocks and minerals of the Kolvitsa massif are studied by complex isotopic–geochronological...crystallization of zircon of metagabbro of the Kolvitsa massif is 778°C. The REE patterns of single zircon...(Cu–Ni, Ti–V, Pt–Pd, etc.) [4]. The Kandalaksha–Kolvitsa Zone of gabbroanorthosites is of great interest...(Fedorovo-Pana, Monchetundra, etc.) [5]. The Kolvitsa gabbroanorthosite massif is located in the southern part of
	Balagansky, V.V, Timmerman, M.J, Kozlova, N.Ye, Kislitsyn, R.V (2001) A 2.44 Ga syn-tectonic mafic dyke swarm in the Kolvitsa Belt, Kola Peninsula, Russia: implications for early Palaeoproterozoic tectonics in the north-eastern Fennoscandian Shield. Precambrian Research, 105 (2) 269-287 doi:10.1016/s0301-9268(00)00115-7	Journal (article/letter/editorial)
	syn-tectonic mafic dyke swarm in the Kolvitsa Belt, Kola Peninsula, Russia: implications for early Palaeoproterozoic...Academy of Sciences, 14 Fersman St., Apatity 184209, Russia b School of Earth Sciences, Leeds Uni6ersity, Leeds...April 1999; accepted 1 November 1999 Abstract The Kolvitsa Belt in the south-western Kola Peninsula formed...gneisses, the intrusion of the 2.45– 2.46 Ga Kolvitsa Massif of gabbro-anorthosite and the subsequent multiple...metamorphism in a compressional setting of the Kolvitsa Belt at 2.45– 2.42 Ga, i.e. coeval with the formation
	Skublov, S. G., Terekhov, E. N. (2009) High-pressure granulites of the Kandalaksha Massif: Geochemistry of minerals and metamorphic conditions. Doklady Earth Sciences, 425 (2) 409-414 doi:10.1134/s1028334x09030131	Journal (article/letter/editorial)
	GEOCHEMISTRY High-Pressure Granulites of the Kandalaksha Massif: Geochemistry of Minerals and Metamorphic Conditions...The Lapland granulite belt (LGB) is considered to be the reference example of granulite-facies metamorphism...conducted for the major northwestern part of the granulite belt [1, 2]. Detailed geological–petrological...the granulites. The Kandalaksha Massif is part of the Kandalaksha–Kolvitsa–Umba segment, which is the isolated...isolated eastern part of the LGB. The massif is an E–W extended synform 40 km long and up to 15 km wide
	Steshenko, Ekaterina N., Bayanova, Tamara B., Serov, Pavel A. (2020) The Paleoproterozoic Kandalaksha-Kolvitsa Gabbro-Anorthosite Complex (Fennoscandian Shield): New U–Pb, Sm–Nd, and Nd–Sr (ID-TIMS) Isotope Data on the Age of Formation, Metamorphism, and Geochemical Features of Zircon (LA-ICP-MS) Minerals, 10 (3) 254 doi:10.3390/min10030254	Journal (article/letter/editorial)
	minerals Article The Paleoproterozoic Kandalaksha-Kolvitsa Gabbro-Anorthosite Complex (Fennoscandian Shield):...Academy of Sciences, Fersman St. 14, 184209 Apatity, Russia; tamara@geoksc.apatity.ru (T.B.B.); serov@geoksc...data on rocks of the Paleoproterozoic Kandalaksha-Kolvitsa gabbro-anorthosite complex. Rare earth element...zircons from basic rock varieties of the Kandalaksha-Kolvitsa area were analyzed in situ using laser ablation...of the Kolvitsa massif. The U–Pb analysis of zircon from anorthosites of the Kandalaksha massif dated
	Reimann, C., Melezhik, V., Niskavaara, H. (2007) LOW-DENSITY REGIONAL GEOCHEMICAL MAPPING OF GOLD AND PALLADIUM HIGHLIGHTING THE EXPLORATION POTENTIAL OF NORTHERNMOST EUROPE. Economic Geology, 102 (2) 327-334 doi:10.2113/gsecongeo.102.2.327	Journal (article/letter/editorial)
	including the western half of the Kola Peninsula, Russia, is well known for its Cu, Ni, PGE, and Au and...Norway (NGU), and the Central Kola Expedition (CKE), Russia, carried out a large, international cooperative...0.17% Co ? C Keivitsa Sodankylä Lapland granulite belt Magmatic Cu, Ni, PGE, Au Regular ore:...Ni ca. 100 U Pahtavaara Sodankylä Lapland granulite belt Mesothermal Au 6.7 ppm Au 0.18->3 A...A Suurikuusikko Kittilä Lapland granulite belt Mesothermal Au 5.4–6.5 ppm Au 0.05–2.2 U Juomasuo
	Fonarev, V. I., Konilov, A. N. (2005) Pulsating Evolution of Metamorphism in Granulite Terrains: Kolvitsa Meta-anorthosite Massif, Kolvitsa Belt, Northeast Baltic Shield. International Geology Review, 47 (8) 815-850 doi:10.2747/0020-6814.47.8.815	Journal (article/letter/editorial)
	of Metamorphism in Granulite Terrains: Kolvitsa Meta-anorthosite Massif, Kolvitsa Belt, Northeast Baltic...of Metamorphism in Granulite Terrains: Kolvitsa Meta-anorthosite Massif, Kolvitsa Belt, Northeast Baltic...of Metamorphism in Granulite Terrains: Kolvitsa Meta-anorthosite Massif, Kolvitsa Belt, Northeast Baltic...Russian Academy of Sciences, 142432 Chernogolovka, Russia Downloaded by [University of York] at 04:03 13...metamorphism of the Kolvitsa meta-anorthosites (metagabbro-anorthosites) (Kolvitsa belt of the Lapland-Kola
	Sharkov, Ye.V. (1977) Layered intrusions of sutural zones of deep-seated faults (as in the gabbro-anorthosite massifs of the Baltic shield) International Geology Review, 19 (1) 66-74 doi:10.1080/00206817709470996	Journal (article/letter/editorial)
	rocks (Archeari) crop out in the Central Kola and Murmansk blocks, often regarded as the basement of the...series, metamorphosed under conditions of the granulite facies of moderate pressures. According to Polkanov...which growth of the Baltic shield took place. The Murmansk block was formed mainly by various granitoids...peninsula where they compose two complexes: 1) the Kolvitsa, Kandalaksha, and Sal'nyye Tundry; and 2) the...studied consists of the White Sea block and two granulite blocks (the Lapland and the Por'ya Guba - Umba)
	Glebovitskii, V. A., Baltybaev, Sh. K., Levchenkov, O. A., Kuz’mina, E. V. (2009) Thermodynamic regime of Svecofennian (1.9 Ga) metamorphism of the Umba nappe of the Lapland collisional orogen. Petrology, 17 (4) 331-351 doi:10.1134/s086959110904002x	Journal (article/letter/editorial)
	Sciences, nab. Makarova 2, St. Petersburg, 190034 Russia e-mail: sb@sb2085spb.edu Received May 27, 2008...after the rocks of the Paleoproterozoic Kolvitsa gabbronorite massif made it possible to trace the P−T evolution...evolution of metamorphsim: the temperature peak of granulite stage (11 kbar, 860°C) was followed by pressure...of the Por’ya Guba nappe together with the Kolvitsa Massif. The U–Pb monazite age of 1904 ± 3 Ma obtained...metamorphic zircon in the anorthosites of the Kolvitsa Massif (1907 ± 2 Ma) and zircon from aluminous gneisses
	Steshenko, E. N., Nikolaev, A. I., Bayanova, T. B., Drogobuzhskaya, S. V., Chashchin, V. V., Serov, P. A., Lyalina, L. M., Novikov, A. I. (2017) The paleoproterozoic Kandalaksha Anorthosite Massif: New U–Pb (ID–TIMS) data and geochemical features of zircon. Doklady Earth Sciences, 477 (2) 1454-1457 doi:10.1134/s1028334x17120194	Journal (article/letter/editorial)
	GEOCHEMISTRY The Paleoproterozoic Kandalaksha Anorthosite Massif: New U–Pb (ID–TIMS) Data and Geochemical Features...isotope data have been obtained in the Kandalaksha–Kolvitsa zone, Baltic Shield, on accessory zircon and rutile...Anorthosite Massif is 2453.5 ± 4.8 Ma, which is close to the U–Pb age of zircon from the Kolvitsa Massif metagabbro...Cu–Ni–PGE (Paleoproterozoic) deposits [5]. The Kolvitsa and Kandalaksha gabbro–anorthosite massifs are...complex isotope–geochemical studies. The Kandalaksha Massif occurs upon the garnet plagio–amphibolite of the
	Khodorevskaya, L. I. (2012) Granulite facies metamorphism and metasomatism in the gabbro-anorthosites of the Kolvitsa massif, Kola Peninsula. Geochemistry International, 50 (3) 272-288 doi:10.1134/s0016702912010041	Journal (article/letter/editorial)
	Geokhimiya, 2012, Vol. 50, No. 3, pp. 298–315 Granulite Facies Metamorphism and Metasomatism in the Gabbro–Anorthosites...Gabbro–Anorthosites of the Kolvitsa Massif, Kola Peninsula L. I. Khodorevskaya Institute of Experimental...Academy of Sciences, Chernogolovka, Moscow oblast, 142432 Russia email: lilia@iem.ac.ru Received December...Abstract—The investigation of the Kolvitsa gabbroanorthosite massif showed that its melanocratic layers...Keywords: Kovitsa massif, gabbro–anorthosite, hightemperature metasomatism, granulite, fluid, basifica
	Glebovitsky, Viktor, Marker, Mogens, Alexejev, Nikolay, Bridgwater, David, Sedova, Irina, Salnikova, Ekaterina, Berezhnaya, Natalia (2001) Age, evolution and regional setting of the Palaeoproterozoic Umba igneous suite in the Kolvitsa–Umba zone, Kola Peninsula: constraints from new geological, geochemical and U–Pb zircon data. Precambrian Research, 105 (2) 247-267 doi:10.1016/s0301-9268(00)00114-5	Journal (article/letter/editorial)
	the Palaeoproterozoic Umba igneous suite in the Kolvitsa–Umba zone, Kola Peninsula: constraints from new...Geology and Geochronology, RAS, St Petersburg, Russia b Geological Sur6ey of Norway, Box 3006, N-7002...charnockite and porphyritic granite which intruded granulite facies paragneisses of the Umba block at the eastern...eastern end of the Palaeoproterozoic Kolvitsa-Umba zone of highgrade gneisses, outcropping on the north...the southeasternmost extension of the Lapland Granulite Belt, which forms the core of the southeast-trending
	*Vetrin, V. R. (2006) Composition and structure of the lower crust of the Belomorian Mobile Belt, Baltic Shield. Petrology, 14 (4) 390-412 doi:10.1134/s0869591106040047*	Journal (article/letter/editorial)
	Sciences, ul. Fersmana 14, Apatity, Murmansk oblast, 184209 Russia e-mail: vetrin@geoksc.apatity.ru Received...high-Mg boninite-like melts metamorphosed to the granulite facies. They form a Paleoproterozoic province...Lapland Granulite Belt, (b) paleorifts (circled numerals): (1) Sal’nye Tundry, (2) Kolvitsa, (3) Imandra–Varzuga...lamprophyre in composition (10–20%). The garnet granulite nodules are 3–10, occasionally up to 40–60 cm...garnet–clinopyroxene rocks. A xenolith of phlogopitized granulite is cut by veinlets of amphibole–clinopyroxene
	Khodorevskaya, L. I., Korikovsky, S. P. (2007) Metasomatic garnet-clinopyroxene-orthopyroxene-hornblende Veins in Metaanorthosites of the Kolvitsa massif, Kola Peninsula: Mineral composition and relation with syngranulite granitization. Doklady Earth Sciences, 415 (2) 915-918 doi:10.1134/s1028334x07060190	Journal (article/letter/editorial)
	Hornblende Veins in Metaanorthosites of the Kolvitsa Massif, Kola Peninsula: Mineral Composition and Relation...in this paper were found within the Kolvitsa anorthosite massif, which experienced metaAbbreviations...Academy of Sciences, Chernogolovka, Moscow oblast, 142432 Russia* b Institute of Geology of Ore Deposits,...Sciences, Staromonetnyi per. 35, Moscow, 119017 Russia; e-mail: lilia@iem.ac morphism and local granitization...granitization (charnockitization) under high-pressure granulite-facies conditions during Svecofennian orogeny
	MINTS, M, KAULINA, T, KONILOV, A, KROTOV, A, STUPAK, V (2007) The thermal and geodynamic evolution of the Lapland granulite belt: Implications for thermal structure of the lower crust during granulite-facies metamorphism. Gondwana Research, 12 (3) 252-267 doi:10.1016/j.gr.2006.10.007	Journal (article/letter/editorial)
	Lapland granulite belt: Implications for thermal structure of the lower crust during granulite-facies...Moscow, Russia Geological Institute, Kola Sci. Center of RAS, Apatity, Murmansk region, Russia c Moscow...State University, Moscow, Russia d SPETSGEOPHYSICA, Povarovka, Moscow region, Russia Received 30 October...Abstract The tectono-thermal history of the Lapland Granulite belt is considered within the framework of a combined... The agreement of thickness estimates of the granulite ensemble obtained from seismic and petrological
	Khodorevskaya, L. I., Varlamov, D. A. (2018) High-Temperature Metasomatism of the Layered Mafic–Ultramafic Massif in Kiy Island, Belomorian Mobile Belt. Geochemistry International, 56 (6) 535-553 doi:10.1134/s001670291806006x	Journal (article/letter/editorial)
	High-Temperature Metasomatism of the Layered Mafic–Ultramafic Massif in Kiy Island, Belomorian Mobile Belt L. I. Khodorevskayaa...Academy of Sciences, Chernogolovka, Moscow oblast, 142432 Russia e-mail: khodorevskaya@mail.ru e-mail:...BMB is the layered peridotite–gabbro–anorthosite massif* cropping out in Kiy Island in the south- ern part...of the Onega Bay of the White Sea (Fig. 1). This massif is likely a fragment of the larger (40 × 20 km)...than 20– 30% mafic minerals. The U–Pb age of the massif is 2.437 Ga (Slabunov et al., 2006). Granatite
	(2006) The Lapland-Kola orogen: Palaeoproterozoic collision and accretion of the northern Fennoscandian lithosphere. Geological Society, London, Memoirs, 32. Geological Society of London. 579-598 doi:10.1144/gsl.mem.2006.032.01.35	Report (chapter)
	Academy of Sciences, 14 Fersman St., Apatity, 184209, Russia 3Institut fiir Geowissenschaften, Universitiit...and sedimentary origin, marked by the Lapland Granulite, Umba and Tersk terranes. Palaeomagnetic data...region of high-P granulite-facies metamorphism, including the classical Lapland Granulite Belt and a broad...orogen (Hjelt et al. 1996) located between the Murmansk and Karelian cratons in the northeastern part...structurally bounded to the north and south by the Murmansk and Karelian cratons, respectively. It is separated
	Sharkov, Evgenii V., Smolkin, Valery F. (1997) The early Proterozoic Pechenga-Varzuga Belt: a case of Precambrian back-arc spreading. Precambrian Research, 82 (1) 133-151 doi:10.1016/s0301-9268(96)00041-1	Journal (article/letter/editorial)
	Academy of Sciences, Staromonetny 35, 109017 Moscow, Russia b Geological Institute, Kola Science Centre of...Academy of Sciences, ul. Fersmana 14, 184200 Apatity, Russia Received 6 March 1995; accepted 14 August 1996...Pechenga-Varzuga Belt (PVB) in the Kola Peninsula, Russia, comprises the western Pechenga and the eastern...southern border of the Paleoproterozoic Lapland-Umba Granulite Belt, and is a narrow zone of compression, thrusting...thrusting and folding accompanied by high-pressure granulite metamorphism. It is approximately coeval with
	Glebovitsky, V. A., Baltybaev, Sh. K., Levchenkov, O. A., Kuz’mina, E. V. (2006) PT-t conditions of metamorphism of the upper and lower parts of the Umba nappe, Baltic Shield. Doklady Earth Sciences, 409 (1) 791-794 doi:10.1134/s1028334x06050266	Journal (article/letter/editorial)
	nappe makes up the upper part of the Kandalaksha–Kolvitsa fragment of the Lapland autochthon [1, 2]. Its...garnet gneisses. The rocks contain the following granulite-facies assemblages: Opx + Cpx + Grt + Hbl + Pl...Sciences, nab. Makarova 2, St. Petersburg, 199034 Russia; e-mail: sb@sb2085.spb.edu lower and upper parts...Kaskeljarvi Complex; (3) Por’ya Guba Complex; (4) Kolvitsa Massif; (5) Kandalaksha Formation; (6) Yauriok and...granite–greenstone terrane. (1) Early Proterozoic granulite belts; (2) mainly mafic rocks beneath the granulites;
	*Turchenko, S.I. (1992) Precambrian metallogeny related to tectonics in the eastern part of the Baltic Shield. Precambrian Research, 58 (1) 121-141 doi:10.1016/0301-9268(92)90116-6*	Journal (article/letter/editorial)
	Academy of Sciences of Russia, nab. Makarova 2, 199034 St. Petersburg, Russia (Received October 5, 1990;...type. The Belomorian Province is a region of granulite-gneiss and granite-greenstone belt terrains reworked...Academy of Sciences of Russia, nab. Makarova 2, 199034 St. Petersburg, Russia. 0301-9268/92/$05.00 ...importance for the mineral resource potential of Russia. However, currently (in 1990) only deposits of...districts and deposits.Tectonic units: 1, 2. Granulite-gneiss terrain of the Kola Peninsula Province
	Korikovsky, S. P., Aranovich, L. Ya. (2015) Charnockitization of feldspar-free orthopyroxene-clinopyroxene-phlogopite metaultramafite in the lapland granulite belt, southern Kola Peninsula: Compositional trends of rocks and minerals, P-T parameters, and fluid regime. Petrology, 23 (3) 189-226 doi:10.1134/s0869591115030030	Journal (article/letter/editorial)
	Clinopyroxene–Phlogopite Metaultramafite in the Lapland Granulite Belt, Southern Kola Peninsula: Compositional Trends...Sciences, Staromonetnyi per. 35, Moscow, 119017 Russia email: korikovsky@yandex.ru, lyaranov@igem.ru...to 6m aureole around the fluid conduit, the granulite has been affected by Na–K–Si–H2O–CO2–Cl–F brine...nebulitic migmatite with skialiths of the modified granulite, then into charnockite migma, and eventually into...Kandalaksha–Umba zone in the southeastern Lapland Granulite Belt, Kola Penin sula. The nappe is one of the
	Volarovich, M.P., Galdin, N.Ye. (1969) Elastic properties of rocks at high pressures; ; granulite massif of Kola peninsula. International Geology Review, 11 (9) 1035-1046 doi:10.1080/00206816909475145	Journal (article/letter/editorial)
	Elastic properties of rocks at high pressures; ; granulite massif of Kola peninsula a M.P. Volarovich & N.Ye...Elastic properties of rocks at high pressures; ; granulite massif of Kola peninsula, International Geology Review... Elastic properties of rocks at high pressures granulite ; massif of Kola peninsula Downloaded by [North Carolina...Baltic shield. I. BRIEF GEOLOGICAL OUTLINE The Granulite massif lies in the western part of the Kola Peninsula;...approximately latitudinal strike (fig. 1). To the west, the massif extends into Finland where it has a generally meridional
	Krivolutskaya, N. A., Belyatsky, B. V., Smolkin, V. F., Mamontov, V. P., Fanygin, A. S., Svirskaya, N. M. (2010) Geochemical specifics of massifs of the drusite complex in the central Belomorian Mobile Belt: II. Sm-Nd isotopic system of the rocks and the U-Pb isotopic system of zircons. Geochemistry International, 48 (11) 1064-1083 doi:10.1134/s0016702910110029	Journal (article/letter/editorial)
	Kosygina 19, Moscow, 119991 Russia email: nakriv@mail.ru b AllRussia Research Institute of Geology...(VNIIOkeanologiya), Angliiskii pr. 1, St. Petersburg, 190121 Russia email: bbelyatsky@mail.ru c Vernadsky State Geological...125007 Russia d Murmansk Geological Exploration OJSC, ul. Fersmana 26, Apatity, 184209 Russia Received...from the Sorkajoki and Poioiva massifs and the massif of Elevation 403 m turned out to be close (within...Belo morie: the intrusions of Pezhostrov Island, Cape Tolstik, Romanovskaya, Voronii Island, YudomNavolok
	Korikovsky, S. P., Aranovich, L. Ya. (2010) Charnockitization and enderbitization of mafic granulites in the Porya Bay area, Lapland Granulite Belt, Southern Kola Peninsula: I. Petrology and geothermobarometry. Petrology, 18 (4) 320-349 doi:10.1134/s0869591110040028	Journal (article/letter/editorial)
	Mafic Granulites in the Porya Bay Area, Lapland Granulite Belt, Southern Kola Peninsula: I. Petrology and...Sciences, Staromonetnyi per. 35, Moscow, 119017 Russia email: korik@igem.ru, lyaranov@igem.ru Received...studied in the southeastern part of the Lapland Granulite Belt. The evolutionary trends of the wholerock...Hbl–Grt–Opx–Cpx–Pl rims were formed along the granulite–charnockite interface, with the bulk composition...veins took place at the peak of the highpressure granulite metamorphism at the same P–T parameters: approximately
	*Krivovichev, Sergey V. - Ed.* (2019) Arctic Mineral Resources. MDPI. doi:10.3390/books978-3-03897-825-1**	Book
	Krivovichev Saint-Petersburg State University Russia Editorial Ofﬁce MDPI St. Alban-Anlage 66 4052...Area and the Salla-Kuolajarvi Zone (Kola Region, Russia) Reprinted from: Minerals 2018, 8, 563, doi:10...of the Kovdor Phoscorite–Carbonatite Complex, NW Russia: I. Forsterite Reprinted from: Minerals 2018, 8...of the Kovdor Phoscorite-Carbonatite Complex, NW Russia: II. Sulﬁdes Reprinted from: Minerals 2018, 8,...of the Kovdor Phoscorite-Carbonatite Complex, NW Russia: III. Pyrochlore Supergroup Minerals Reprinted
	Khodorevskaya, L. I. (2020) Experimental Study of Amphibole Interaction with H2O–HCl Fluid at 650–750°C, 5–7 Kbar: Implications for High-Temperature Metasomatism of Metabasites. Geochemistry International, 58 (7) 779-794 doi:10.1134/s001670292007006x	Journal (article/letter/editorial)
	Academy of Sciences, Chernogolovka, Moscow oblast, 142432 Russia e-mail: khodorevskaya@mail.ru Received...amphibole of the metasomatites, amphibole in the host granulite-facies metabasites is not as rich in Fe (XFe ≤...high-temperature metasomatism under amphibolite- and granulite-facies parameters. 1 Mineral symbols: Ab—albite...a closed system, the layered gabbro–anorthosite massif* at Kii Island was an open system. Lenses with corundum...leucocratic beds of the peridotite–gabbro– anorthosite massif at Kii Island. Our experimental results, for example

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Granulite from Kolvitsa massif, Kataranskii Cape, Murmansk Oblast, Russia

Granulite from
Kolvitsa massif, Kataranskii Cape, Murmansk Oblast, Russia