gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0292gtcrust-433Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSGEOCHEMISTRY, ZIRCON U-PB GEOCHRONOLOGY, ND-HF ISOTOPIC CHARACTERISTICS AND TECTONIC IMPLICATIONS OF THE SOUTH MUYA BLOCK METASEDIMENTS (NORTHEASTERN CENTRAL ASIAN OROGENIC BELT)GEOCHEMISTRY, ZIRCON U-PB GEOCHRONOLOGY, ND-HF ISOTOPIC CHARACTERISTICS AND TECTONIC IMPLICATIONS OF THE SOUTH MUYA BLOCK METASEDIMENTS (NORTHEASTERN CENTRAL ASIAN OROGENIC BELT)SkuzovatovS. Yu.SkuzovatovS. Yu.

Irkutsk

Irkutsk

NoskovaYu. V.NoskovaYu. V.

Irkutsk

Irkutsk

DrilS. I.DrilS. I.

Irkutsk

Irkutsk

WangK.-L.WangK.-L.

Taipei

Taipei

IizukaY.IizukaY.

Taipei

Taipei

A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASРоссияA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASRussian FederationInstitute of Earth Sciences, Academia SinicaТайваньInstitute of Earth Sciences, Academia SinicaTaiwan, Province of China20171310201783565568Copyright © Skuzovatov S.Y., Noskova Y.V., Dril S.I., Wang K., Iizuka Y., 20172017Skuzovatov S.Y., Noskova Y.V., Dril S.I., Wang K., Iizuka Y.Skuzovatov S.Y., Noskova Y.V., Dril S.I., Wang K., Iizuka Y.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/433

The Neoproterozoic to Cenozoic collage of the Central Asian Orogenic Belt is well-known to include Precambrian continental blocks and microcontinents traditionally attributed to rifting of Siberia or Gondwana prior to CAOB assembly that significantly contributed into the geochemical and isotopic composition of younger subduction- and accretion-related crustal lithologies via processes of crust-mantle interaction and crustal recycling.

The Neoproterozoic to Cenozoic collage of the Central Asian Orogenic Belt is well-known to include Precambrian continental blocks and microcontinents traditionally attributed to rifting of Siberia or Gondwana prior to CAOB assembly that significantly contributed into the geochemical and isotopic composition of younger subduction- and accretion-related crustal lithologies via processes of crust-mantle interaction and crustal recycling.

Russian Federation President FoundationReferencesShatskii V.S., Skuzovatov S.Yu., Ragozin A.L., Dril S.I., 2014. Evidence of Neoproterosoic continental subduction in the Baikal-Muya Fold belt. Doklady Earth Sciences 459 (1), 1442–1445. https://doi.org/10.1134/S1028334X14110166.Shatskii V.S., Skuzovatov S.Yu., Ragozin A.L., Dril S.I., 2014. Evidence of Neoproterosoic continental subduction in the Baikal-Muya Fold belt. Doklady Earth Sciences 459 (1), 1442–1445. https://doi.org/10.1134/S1028334X14110166.Shatsky V.S., Malkovets V.G., Belousova E.A., Skuzovatov S.Yu., 2015. Evolution history of the Neoproterozoic eclogitebearing complex of the Muya dome (Central Asian Orogenic Belt): constraints from zircon U-Pb age, Hf and wholerock Nd isotopes. Precambrian Research 261, 1–11. https://doi.org/10.1016/j.precamres.2015.01.013.Shatsky V.S., Malkovets V.G., Belousova E.A., Skuzovatov S.Yu., 2015. Evolution history of the Neoproterozoic eclogitebearing complex of the Muya dome (Central Asian Orogenic Belt): constraints from zircon U-Pb age, Hf and wholerock Nd isotopes. Precambrian Research 261, 1–11. https://doi.org/10.1016/j.precamres.2015.01.013.Skuzovatov S.Yu., Sklyarov E.V., Shatsky V.S., Wang K.-L., Kulikova K.V., Zarubina O.V., 2016a. Granulites of the SouthMuya block (Baikal-Muya Foldbelt): age of metamorphism and nature of protolith. Russian Geology and Geophysics 57 (3), 451–463. https://doi.org/10.1016/j.rgg.2016.03.007.Skuzovatov S.Yu., Sklyarov E.V., Shatsky V.S., Wang K.-L., Kulikova K.V., Zarubina O.V., 2016a. Granulites of the SouthMuya block (Baikal-Muya Foldbelt): age of metamorphism and nature of protolith. Russian Geology and Geophysics 57 (3), 451–463. https://doi.org/10.1016/j.rgg.2016.03.007.Skuzovatov S.Yu., Wang K.-L., Shatsky V.S., Buslov M.M., 2016b. Geochemistry, zircon U-Pb age and Hf isotopes of the North Muya block granitoids (Central Asian Orogenic belt): constraints on petrogenesis and geodynamic significance of felsic magmatism. Precambrian Research 280, 14–30. https://doi.org/10.1016/j.precamres.2016.04.015.Skuzovatov S.Yu., Wang K.-L., Shatsky V.S., Buslov M.M., 2016b. Geochemistry, zircon U-Pb age and Hf isotopes of the North Muya block granitoids (Central Asian Orogenic belt): constraints on petrogenesis and geodynamic significance of felsic magmatism. Precambrian Research 280, 14–30. https://doi.org/10.1016/j.precamres.2016.04.015.Skuzovatov S.Yu., Shatsky V.S., Dril S.I., 2017. High-pressure mafic granulites of the South Muya block (Central Asian Orogenic Belt). Doklady Earth Sciences 473 (2), 423–426. https://doi.org/10.1134/S1028334X17040067.Skuzovatov S.Yu., Shatsky V.S., Dril S.I., 2017. High-pressure mafic granulites of the South Muya block (Central Asian Orogenic Belt). Doklady Earth Sciences 473 (2), 423–426. https://doi.org/10.1134/S1028334X17040067.

The authors declare that there are no conflicts of interest present.