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High-pressure mafic granulites of the South Muya Block (Central Asian Orogenic Belt). / Skuzovatov, S. Yu; Shatsky, V. S.; Dril, S. I.

In: Doklady Earth Sciences, Vol. 473, No. 2, 01.04.2017, p. 423-426.

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

Harvard

Skuzovatov, SY, Shatsky, VS & Dril, SI 2017, 'High-pressure mafic granulites of the South Muya Block (Central Asian Orogenic Belt)', Doklady Earth Sciences, vol. 473, no. 2, pp. 423-426. https://doi.org/10.1134/S1028334X17040067

APA

Skuzovatov, S. Y., 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

Vancouver

Skuzovatov SY, Shatsky VS, Dril SI. High-pressure mafic granulites of the South Muya Block (Central Asian Orogenic Belt). Doklady Earth Sciences. 2017 Apr 1;473(2):423-426. doi: 10.1134/S1028334X17040067

Author

Skuzovatov, S. Yu ; Shatsky, V. S. ; Dril, S. I. / High-pressure mafic granulites of the South Muya Block (Central Asian Orogenic Belt). In: Doklady Earth Sciences. 2017 ; Vol. 473, No. 2. pp. 423-426.

BibTeX

@article{6fbc7faefa7e45dfb664d0d0097cba36,
title = "High-pressure mafic granulites of the South Muya Block (Central Asian Orogenic Belt)",
abstract = "Mineralogical, petrographic, and geochemical studies of mafic granulites of the South Muya Block (Central Asian Orogenic Belt) have been carried out. The granulite protoliths were olivine- and plagioclase- rich cumulates of ultramafic–mafic magmas with geochemical affinities of suprasubduction rocks. The isotope–geochemical characteristics of the granulites indicate the enriched nature of their source, associated with recycling into the mantle of either ancient crust or oceanic sediments, or intracrustal contamination of melts at the basement of the ensialic arc. Formation of garnet-bearing parageneses has occurred during high-pressure granulite metamorphism associated with accretion in the eastern part of the Baikal–Muya composite terrane.",
author = "Skuzovatov, {S. Yu} and Shatsky, {V. S.} and Dril, {S. I.}",
year = "2017",
month = apr,
day = "1",
doi = "10.1134/S1028334X17040067",
language = "English",
volume = "473",
pages = "423--426",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - High-pressure mafic granulites of the South Muya Block (Central Asian Orogenic Belt)

AU - Skuzovatov, S. Yu

AU - Shatsky, V. S.

AU - Dril, S. I.

PY - 2017/4/1

Y1 - 2017/4/1

N2 - Mineralogical, petrographic, and geochemical studies of mafic granulites of the South Muya Block (Central Asian Orogenic Belt) have been carried out. The granulite protoliths were olivine- and plagioclase- rich cumulates of ultramafic–mafic magmas with geochemical affinities of suprasubduction rocks. The isotope–geochemical characteristics of the granulites indicate the enriched nature of their source, associated with recycling into the mantle of either ancient crust or oceanic sediments, or intracrustal contamination of melts at the basement of the ensialic arc. Formation of garnet-bearing parageneses has occurred during high-pressure granulite metamorphism associated with accretion in the eastern part of the Baikal–Muya composite terrane.

AB - Mineralogical, petrographic, and geochemical studies of mafic granulites of the South Muya Block (Central Asian Orogenic Belt) have been carried out. The granulite protoliths were olivine- and plagioclase- rich cumulates of ultramafic–mafic magmas with geochemical affinities of suprasubduction rocks. The isotope–geochemical characteristics of the granulites indicate the enriched nature of their source, associated with recycling into the mantle of either ancient crust or oceanic sediments, or intracrustal contamination of melts at the basement of the ensialic arc. Formation of garnet-bearing parageneses has occurred during high-pressure granulite metamorphism associated with accretion in the eastern part of the Baikal–Muya composite terrane.

UR - http://www.scopus.com/inward/record.url?scp=85019359382&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17040067

DO - 10.1134/S1028334X17040067

M3 - Article

AN - SCOPUS:85019359382

VL - 473

SP - 423

EP - 426

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 10036534