Skip to main content
Log in

Three metamorphic events in the precambrian P-T-t history of the Transangarian Yenisey ridge recorded in garnet grains in metapelites

  • Published:
Petrology Aims and scope Submit manuscript

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.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

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.

    Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • Brown, M., Metamorphic conditions in orogenic belts: a record of secular change, Int. Geol. Rev., 2007, vol. 49, pp. 193–234.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • Dobretsov, N.L., Global geodynamic evolution of the Earth and global geodynamic models, Russ. Geol. Geophys., 2010, vol. 51, no. 6, pp. 592–610.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • Gerya, T.V., Precambrian geodynamics: concepts and models, Gondwana Res., 2012. doi: http://dx.doi.org/10.1016/j.gr.2012.11.008.

    Google Scholar 

  • Hodges, K.V. and Crowley, P.D., Error estimation and empirical geothermobarometry for pelitic system, Am. Mineral., 1985, vol. 70, pp. 702–709.

    Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Google Scholar 

  • Holdaway, M.J., Application of new experimental and garnet Margules data to the garnet-biotite geothermometer, Am. Mineral., 2000, vol. 85, pp. 881–889.

    Google Scholar 

  • 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.

    Article  Google Scholar 

  • Kaneko, Y. and Miyano, T., Recalibration of mutually consistent garnet-biotite and garnet-cordierite geothermometers, Lithos, 2004, vol. 73, pp. 255–269.

    Article  Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Article  Google Scholar 

  • Powell, R. and Holland, T.J.B., Optimal geothermometry and geobarometry, Am. Mineral., 1994, vol. 79, pp. 120–133.

    Google Scholar 

  • 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.

    Google Scholar 

  • Sklyarov, E.V., Exhumation of metamorphic complexes: basic mechanisms, Russ. Geol. Geophys., 2006, vol. 47, no. 1, pp. 68–72.

    Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

  • Whitney, D.L. and Evans, B.W., Abbreviations for names of rock-forming minerals, Am. Mineral., 2010, vol. 95, pp. 185–187.

    Article  Google Scholar 

  • 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.

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to I. I. Likhanov.

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

Reprints 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

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1134/S0869591113060040

Keywords

Navigation