Abstract
A study of gneisses and schists from the Yenisey regional shear zone (Garevka complex) at the western margin of the Siberian Craton has provided important constraints on the tectonothermal events and geodynamic processes in the Yenisey Ridge during the Riphean. In situ U-Th-Pb geochronology of monazite and xenotime from different garnet growth zones and the calculation of P-T path derived from chemical zoning pattern in garnet were used to distinguish three metamorphic events with different ages, thermodynamic regimes and metamorphic field gradients. The first stage occurred as a result of the Grenville orogeny during late Meso-early Neoproterozoic (1050–850 Ma) and was marked by low-pressure zoned metamorphism at ∼4.8–5.0 kbar and 565–580°C and a metamorphic field gradient with dT/dH = 20–30°C/km typical of orogenic belts. At the second stage, the rocks experienced Late Riphean (801–793 Ma) collision-related medium-pressure metamorphism at ∼7.7–7.9 kbar and 630°C with dT/dH ≤ 10°C/km. The final stage evolved as a syn-exhumation retrograde metamorphism (785–776 Ma) at ∼4.8–5.4 kbar and 500°C with dT/dH ≤ 12°C/km and recorded a relatively fast uplift of the rocks to upper crustal levels in shear zones. The range of exhumation rates at the post-collisional stage (500–700 m/Ma) correlates with the duration of exhumation and the results of thermophysical numerical modeling of metamorphic rocks within orogenic belts. The final stages of collisional orogeny are marked by the development of rift-related bimodal dyke swarms associated with Neoproterozoic extension (797 ± 11 and 7.91 ± 6 Ma; U-Pb SHRIMP II zircon data) along the western margin of the Siberian craton and the beginning of the breakup of Rodinia. Post-Grenville metamorphic episodes of regional evolution are correlated with the synchronous succession and similar style of the later tectono-metamorphic events within the Valhalla orogen along the Arctic margin of Rodinia and support the spatial proximity of Siberia and North Atlantic cratons at about 800 Ma, as indicated by the latest paleomagnetic reconstructions.
Similar content being viewed by others
References
Berman, R.G., Thermobarometry using multi-equilibrium calculations: a new technique with petrological applications, Can. Mineral., 1991, vol. 29, pp. 833–855.
Berman, R.G. and Aranovich, L.Y., Optimized standard state and solution properties of minerals, Contrib. Mineral. Petrol., 1996, vol. 126, nos. 1–2, pp. 1–24.
Bestel, M., Gawronski, T., Abart, R., and Rhede, D., Compositional zoning of garnet porphyroblasts from the polymetamorphic Wölz Complex, Eastern Alps, Mineral. Petrol, 2009, vol. 97, pp. 173–188.
Bogdanova, S.V., Pisarevskii, S.A., and Li, Z.X., Assembly and Breakup of Rodinia (Some Results of IGCP Project 440), Stratigr. Geol. Correlation, 2009, vol. 17, no. 3, pp. 259–274.
Brown, M., Metamorphic conditions in orogenic belts: a record of secular change, Int. Geol. Rev., 2007, vol. 49, pp. 193–234.
Cawood, P.A., Strachan, R., Cutts, K., et al., Neoproterozoic orogeny along the margin of Rodinia: Valhalla orogen, North Atlantic, Geology, 2010, vol. 38, no. 2, pp. 99–102.
Cutts, K.A., Kinny, P.D., Strachan, R.A., et al., Three metamorphic events recorded in a single garnet: integrated phase modelling, in situ LA-ICPMS and SIMS geochronology from the Moine Supergroup, NW Scotland, J. Metamorph. Geol, 2010, vol. 28, pp. 249–267.
Dalziel, I.W.D., Mosher, S., and Gahagan, L.M., Laurentia-Kalahari collision and the assembly of Rodinia, J. Geol., 2000, vol. 108, pp. 499–513.
Dobretsov, N.L., Global geodynamic evolution of the Earth and global geodynamic models, Russ. Geol. Geophys., 2010, vol. 51, no. 6, pp. 592–610.
Ferry, J.M. and Spear, F.S., Experimental calibration of the partitioning of Fe and Mg between biotite and garnet, Contrib. Mineral. Petrol., 1978, vol. 66, pp. 113–117.
Gerya, T.V., Precambrian geodynamics: concepts and models, Gondwana Res., 2012. doi: http://dx.doi.org/10.1016/j.gr.2012.11.008.
Hodges, K.V. and Crowley, P.D., Error estimation and empirical geothermobarometry for pelitic system, Am. Mineral., 1985, vol. 70, pp. 702–709.
Hoisch, T.D., Empirical calibration of six geobarometers for the mineral assemblage quartz + muscovite + biotite + plagioclase + garnet, Contrib. Mineral. Petrol., 1990, vol. 104, pp. 225–234.
Holdaway, M.J., Mukhopadhyay, B., Dyar, M.D., et al., Garnet-biotite geothermometry revised: New Margules parameters and a natural specimen data set from Maine, Am. Mineral., 1997, vol. 82, pp. 582–595.
Holdaway, M.J., Application of new experimental and garnet Margules data to the garnet-biotite geothermometer, Am. Mineral., 2000, vol. 85, pp. 881–889.
Holland, T.J.B. and Powell, R., An internally consistent thermodynamic data set for phases of petrological interest, J. Metamorph. Geol, 1998, vol. 16, pp. 309–343.
Kaneko, Y. and Miyano, T., Recalibration of mutually consistent garnet-biotite and garnet-cordierite geothermometers, Lithos, 2004, vol. 73, pp. 255–269.
Kleemann, U. and Reinhardt, J., Garnet-biotite thermometry revisited: the effect of AlVI and Ti in biotite, Eur. J. Mineral., 1994, vol. 6, pp. 925–941.
Kozlov, P.S., Likhanov, I.I., Reverdatto, V.V., and Zinov’ev, S.V., Tectonometamorphic evolution of the Garevka polymetamorphic complex (Yenisei Ridge), Russ. J. Geol. Geophys., 2012, vol. 53, no. 11, pp. 1133–1149.
Likhanov, I.I., Reverdatto, V.V., and Memmi, I., Short-range mobilization of elements in the biotite zone of contact aureole of the Kharlovo gabbro massif (Russia), Eur. J. Mineral., 1994, vol. 6, pp. 133–144.
Likhanov, I.I., Reverdatto, V.V., Sheplev, V.S., et al., Contact metamorphism of Fe- and Al-rich graphitic metapelites in the Transangarian region of the Yenisey Ridge, eastern Siberia, Russia, Lithos, 2001, vol. 58, pp. 55–80.
Likhanov, I.I. and Reverdatto, V.V., Mass transfer during andalusite replacement by kyanite in Al- and Fe-rich metapelites in the Yenisei Range, Petrology, 2002, vol. 10, no. 5, pp. 479–494.
Likhanov, I.I., Polyansky, O.P., Reverdatto, V.V., and Memmi, I., Evidence from Fe- and Al-rich metapelites for thrust loading in the Transangarian region of the Yenisey Ridge, eastern Siberia, J. Metamorph. Geol, 2004, vol. 22, pp. 743–762.
Likhanov, I.I., Reverdatto, V.V., and Selyatitskii, A.Yu., Mineral equilibria and P-T diagram for Fe-Al metapelites in the KFMASH system (K2O-FeO-MgO-Al2O3-SiO2-H2O), Petrology, 2005, vol. 13, no. 1, pp. 73–83.
Likhanov, I.I., Kozlov, P.S., Popov, N.V., et al., Collisional metamorphism as a result of thrusting in the Transangara region of the Yenisei Ridge, Dokl. Earth Sci., 2006, vol. 411, no. 8, pp. 1313–1317.
Likhanov, I.I. and Reverdatto, V.V., Provenance of Precambrian Fe- and Al-rich metapelites in the Yenisey Ridge and Kuznetsk Alatau, Siberia: geochemical signatures, Acta Geol. Sinica-English Edition, 2007, vol. 81, pp. 409–423.
Likhanov, I.I. and Reverdatto, V.V., Precambrian Fe- and Al-rich pelites from the Yenisey Ridge, Siberia: geochemical signatures for protolith origin and evolution during metamorphism, Int. Geol. Rev., 2008, vol. 50, pp. 597–623.
Likhanov, I.I., Reverdatto, V.V., Kozlov, P.S., and Popov, N.V., Collision metamorphism of Precambrian complexes in the Transangarian Yenisei Range, Petrology, 2008, vol. 16, no. 2, pp. 136–160.
Likhanov, I.I., Reverdatto, V.V., Kozlov, P.S., and Popov, N.V., Kyanite-sillimanite metamorphism of the Precambrian complexes, Transangarian region of the Yenisei Range, Russ. Geol. Geophys., 2009, vol. 50, pp. 1034–1051.
Likhanov, I.I. and Reverdatto, V.V., Lower Proterozoic metapelites in the Northern Yenisei Range: nature and age of the protolith and the behavior of material during collisional metamorphism, Geochem. Int., 2011, vol. 49, no. 3, pp. 224–252.
Likhanov, I.I. and Reverdatto, V.V., Neoproterozoic collisional metamorphism in overthrust terranes of the Transangarian Yenisey Ridge, Siberia, Int. Geol. Rev., 2011, vol. 53, pp. 802–845.
Likhanov, I.I., Reverdatto, V.V., and Kozlov, P.S., Collision-related metamorphic complexes of the Yenisei Ridge: their evolution, ages, and exhumation rate, Russ. Geol. Geophys., 2011, vol. 52, no. 10, pp. 1256–1269.
Likhanov, I.I., Reverdatto, V.V., and Kozlov, P.S., U-Pb and 40Ar/39Ar evidence for Grenvillian activity in the Yenisey Ridge during formation of the Teya metamorphic vomplex, Geochem. Int., 2012a, vol. 50, no. 6, pp. 551–557.
Likhanov, I.I., Reverdatto, V.V., Popov, N.V., and Kozlov, P.S., The First Find of Rapakivi Granite in the Yenisei Ridge: Age, P-T Conditions, and Tectonic Settings, Dokl. Earth Sci., 2012b, vol. 443, no. 1, pp. 365–370.
Likhanov, I.I., Reverdatto, V.V., Kozlov, P.S., and Khiller, V.V., Neoproterozoic metamorphic evolution in the Transangarian Yenisei Ridge: evidence from monazite and xenotime geochronology, Dokl. Earth Sci., 2013, vol. 450, no. 1, pp. 556–561.
Maruyama, S., Santosh, M., and Zhao, D., Superplume, supercontinent, and post-perovskite: mantle dynamics and anti-plate tectonics on the core-mantle boundary, Gondwana Res., 2007, vol. 11, pp. 7–37.
Nozhkin, A.D., Borisenko, A.S., and Nevol’ko, P.A., Stages of Late Proterozoic magmatism and periods of Au mineralization in the Yenisei Ridge, Russ. Geol. Geophys., 2011, vol. 52, no. 1, pp. 124–142.
Pattison, D.R.M., Instability of Al2SiO5 “triple point” assemblages in muscovite + biotite + quartz-bearing metapelites, with implications, Am. Mineral., 2001, vol. 86, pp. 1414–1422.
Perchuk, L.L. and Lavrent’eva, I.V., in Kinetics and equilibrium in mineral reactions, Saxena, S.K., Ed., Berlin-Heidelberg-New York: Springer, 1983, pp. 199–239.
Popov, N.V., Likhanov, I.I., and Nozhkin, A.D., Mesoproterozoic granitoid magmatism in the Trans-Angara Segment of the Yenisei Range: U-Pb evidence, Dokl. Earth Sci., 2010, vol. 431, no. 2, pp. 418–423.
Powell, R. and Holland, T.J.B., Optimal geothermometry and geobarometry, Am. Mineral., 1994, vol. 79, pp. 120–133.
Sizova, E.V., Gerya, T.V., and Brown, M., Contrasting styles of Phanerozoic and Precambrian continental collision, Gondwana Res., 2012.; doi: http://dx.doi.org/10.1016/j.gr.2012.12.011.
Sklyarov, E.V., Exhumation of metamorphic complexes: basic mechanisms, Russ. Geol. Geophys., 2006, vol. 47, no. 1, pp. 68–72.
Spear, F.S., Peacock, S.M., Kohn, M.J., and Florence, F., Computer programs for petrologic P-T-t path calculations, Am. Mineral., 1991, vol. 76, pp. 2009–2012.
Spear, F.S., Kohn, M.J., Cheney, J.T., and Florence, F., Metamorphic, thermal, and tectonic evolution of central New England, J. Petrol., 2002, vol. 43, pp. 2097–2120.
Suzuki, K. and Kato, T., CHIME dating of monazite, xenotime, zircon and polycrase: protocol, pitfalls and chemical criterion of possibly discordant age data, Gondwana Res., 2008, vol. 14, pp. 569–586.
Vernikovsky, V.A., Vernikovskaya, A.E., Polyansky, O.P., et al., A tectonothermal model for the formation of an orogen at the postcollisional stage (by the example of the Yenisei Ridge, East Siberia), Russ. Geol. Geophys., 2011, vol. 52, no. 1, pp. 24–39.
Whitney, D.L. and Evans, B.W., Abbreviations for names of rock-forming minerals, Am. Mineral., 2010, vol. 95, pp. 185–187.
Wu, C.M., Zhang, J., and Ren, L.D., Empirical garnetbiotite-plagioclase-quartz (QBPQ) geobarometry in medium- to high-grade metapelites, J. Petrol., 2004, vol. 45, no. 9, pp. 1907–1921.
Author information
Authors and Affiliations
Corresponding author
Additional information
Original Russian Text © I.I. Likhanov, V.V. Reverdatto, P.S. Kozlov, V.V. Khiller, V.P. Sukhorukov, 2013, published in Petrologiya, 2013, Vol. 21, No. 6, pp. 612–631.
Rights and permissions
About this article
Cite this article
Likhanov, I.I., Reverdatto, V.V., Kozlov, P.S. et al. Three metamorphic events in the precambrian P-T-t history of the Transangarian Yenisey ridge recorded in garnet grains in metapelites. Petrology 21, 561–578 (2013). https://doi.org/10.1134/S0869591113060040
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1134/S0869591113060040