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Granulites of the South Muya block (Baikal-Muya Foldbelt) : Age of metamorphism and nature of protolith. / Skuzovatov, S. Yu; Sklyarov, E. V.; Shatsky, V. S. et al.

In: Russian Geology and Geophysics, Vol. 57, No. 3, 01.03.2016, p. 451-463.

Research output: Contribution to journal › Article › peer-review

Harvard

Skuzovatov, SY, Sklyarov, EV, Shatsky, VS, Wang, KL, Kulikova, KV & Zarubina, OV 2016, 'Granulites of the South Muya block (Baikal-Muya Foldbelt): Age of metamorphism and nature of protolith', Russian Geology and Geophysics, vol. 57, no. 3, pp. 451-463. https://doi.org/10.1016/j.rgg.2016.03.007

APA

Skuzovatov, S. Y., Sklyarov, E. V., Shatsky, V. S., Wang, K. L., Kulikova, K. V., & Zarubina, O. V. (2016). Granulites of the South Muya 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

Vancouver

Skuzovatov SY, Sklyarov EV, Shatsky VS, Wang KL, Kulikova KV, Zarubina OV. Granulites of the South Muya block (Baikal-Muya Foldbelt): Age of metamorphism and nature of protolith. Russian Geology and Geophysics. 2016 Mar 1;57(3):451-463. doi: 10.1016/j.rgg.2016.03.007

Author

Skuzovatov, S. Yu ; Sklyarov, E. V. ; Shatsky, V. S. et al. / Granulites of the South Muya block (Baikal-Muya Foldbelt) : Age of metamorphism and nature of protolith. In: Russian Geology and Geophysics. 2016 ; Vol. 57, No. 3. pp. 451-463.

BibTeX

@article{8666c4ac84d54614bee96b2406c4db05,
title = "Granulites of the South Muya block (Baikal-Muya Foldbelt): Age of metamorphism and nature of protolith",
abstract = "High-pressure mafic granulites and garnet pyroxenites occur within the South Muya block as boudins or lenses among metamorphic rocks of the Kindikan Group. Their primary minerals crystallized at 670-750 °C and 9.5-12.0 kbar. Granulite metamorphism peaked at 630 Ma, according to LA-ICP-MS U-Pb zircon ages. Judging by their major- and trace-element compositions and Hf isotope ratios in zircons, the South Muya granulites were derived from differentiated within-plate basalts, which, in turn, resulted from melting of juvenile mantle source and Meso- or Paleoproterozoic crust. The events of granulite and eclogite metamorphism in the South and North Muya blocks, respectively, were coeval and the two blocks were spatially close to each other at the onset of Late Baikalian subduction and collision events.",
keywords = "Central Asian Orogenic Belt, Continental subduction, Garnet pyroxenites, Granulites, South Muya block, U-Pb age, Zircon",
author = "Skuzovatov, {S. Yu} and Sklyarov, {E. V.} and Shatsky, {V. S.} and Wang, {K. L.} and Kulikova, {K. V.} and Zarubina, {O. V.}",
year = "2016",
month = mar,
day = "1",
doi = "10.1016/j.rgg.2016.03.007",
language = "English",
volume = "57",
pages = "451--463",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "3",

}

RIS

TY - JOUR

T1 - Granulites of the South Muya block (Baikal-Muya Foldbelt)

T2 - Age of metamorphism and nature of protolith

AU - Skuzovatov, S. Yu

AU - Sklyarov, E. V.

AU - Shatsky, V. S.

AU - Wang, K. L.

AU - Kulikova, K. V.

AU - Zarubina, O. V.

PY - 2016/3/1

Y1 - 2016/3/1

N2 - High-pressure mafic granulites and garnet pyroxenites occur within the South Muya block as boudins or lenses among metamorphic rocks of the Kindikan Group. Their primary minerals crystallized at 670-750 °C and 9.5-12.0 kbar. Granulite metamorphism peaked at 630 Ma, according to LA-ICP-MS U-Pb zircon ages. Judging by their major- and trace-element compositions and Hf isotope ratios in zircons, the South Muya granulites were derived from differentiated within-plate basalts, which, in turn, resulted from melting of juvenile mantle source and Meso- or Paleoproterozoic crust. The events of granulite and eclogite metamorphism in the South and North Muya blocks, respectively, were coeval and the two blocks were spatially close to each other at the onset of Late Baikalian subduction and collision events.

AB - High-pressure mafic granulites and garnet pyroxenites occur within the South Muya block as boudins or lenses among metamorphic rocks of the Kindikan Group. Their primary minerals crystallized at 670-750 °C and 9.5-12.0 kbar. Granulite metamorphism peaked at 630 Ma, according to LA-ICP-MS U-Pb zircon ages. Judging by their major- and trace-element compositions and Hf isotope ratios in zircons, the South Muya granulites were derived from differentiated within-plate basalts, which, in turn, resulted from melting of juvenile mantle source and Meso- or Paleoproterozoic crust. The events of granulite and eclogite metamorphism in the South and North Muya blocks, respectively, were coeval and the two blocks were spatially close to each other at the onset of Late Baikalian subduction and collision events.

KW - Central Asian Orogenic Belt

KW - Continental subduction

KW - Garnet pyroxenites

KW - Granulites

KW - South Muya block

KW - U-Pb age

KW - Zircon

UR - http://www.scopus.com/inward/record.url?scp=84962163501&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.03.007

DO - 10.1016/j.rgg.2016.03.007

M3 - Article

AN - SCOPUS:84962163501

VL - 57

SP - 451

EP - 463

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 3

ER -

ID: 25794608