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Late Neoproterozoic adakites of the Yenisei Ridge (Central Siberia) : petrogenesis, geodynamics, and U/Pb age. / Vernikovskaya, A. E.; Vernikovsky, V. A.; Matushkin, N. Yu et al.

In: Russian Geology and Geophysics, Vol. 58, No. 10, 01.10.2017, p. 1154-1170.

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Vernikovskaya AE, Vernikovsky VA, Matushkin NY, Kadil'nikov PI, Romanova IV, Larionov AN. Late Neoproterozoic adakites of the Yenisei Ridge (Central Siberia): petrogenesis, geodynamics, and U/Pb age. Russian Geology and Geophysics. 2017 Oct 1;58(10):1154-1170. doi: 10.1016/j.rgg.2016.12.008

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@article{20398de5ba90427899e0080d91d4d01c,
title = "Late Neoproterozoic adakites of the Yenisei Ridge (Central Siberia): petrogenesis, geodynamics, and U/Pb age",
abstract = "Based on new geological, structural, mineralogical, geochemical, and isotope (Sm-Nd, Rb-Sr, and U-Th-Pb) data for igneous intrusions and metamorphic rocks of the Zimoveinyi massif, an adakite-gabbroid association was identified for the first time in the Yenisei Ridge (southwestern framing of the Siberian craton). This study demonstrates that the adakites (quartz diorites, tonalites, and plagiogranites) and associating gabbro-anorthosites of this massif formed in the interval 576-546 Ma (U-Th-Pb zircon SHRIMP-II analysis) at the final Neoproterozoic evolution stage of the active continental margin of the Siberian craton. Our results point to a genetic relationship between the adakites and the host Nb-enriched metabasites of the Zimoveinyi massif. The studied late Neoproterozoic adakites might have formed in the setting of transform strike-slip of lithospheric plates during a halt in subduction from both crustal and mantle-crustal source, similarly to Cenozoic igneous complexes of the transform margin in the eastern framing of Eurasia.",
keywords = "active and transform continental margin, adakites, gabbro-anorthosites, late Neoproterozoic, Nb-enriched metabasites, Rb-Sr isotope data, Siberian craton, Sm-Nd, U-Th-Pb, Yenisei Ridge, NB-ENRICHED BASALTS, EVENTS, ALKALINE MAGMATISM, SUBDUCTION, WESTERN MARGIN, NOMENCLATURE, EVOLUTION, CRATON, GEOCHEMISTRY, PALEOMAGNETIC DATA",
author = "Vernikovskaya, {A. E.} and Vernikovsky, {V. A.} and Matushkin, {N. Yu} and Kadil'nikov, {P. I.} and Romanova, {I. V.} and Larionov, {A. N.}",
year = "2017",
month = oct,
day = "1",
doi = "10.1016/j.rgg.2016.12.008",
language = "English",
volume = "58",
pages = "1154--1170",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "10",

}

RIS

TY - JOUR

T1 - Late Neoproterozoic adakites of the Yenisei Ridge (Central Siberia)

T2 - petrogenesis, geodynamics, and U/Pb age

AU - Vernikovskaya, A. E.

AU - Vernikovsky, V. A.

AU - Matushkin, N. Yu

AU - Kadil'nikov, P. I.

AU - Romanova, I. V.

AU - Larionov, A. N.

PY - 2017/10/1

Y1 - 2017/10/1

N2 - Based on new geological, structural, mineralogical, geochemical, and isotope (Sm-Nd, Rb-Sr, and U-Th-Pb) data for igneous intrusions and metamorphic rocks of the Zimoveinyi massif, an adakite-gabbroid association was identified for the first time in the Yenisei Ridge (southwestern framing of the Siberian craton). This study demonstrates that the adakites (quartz diorites, tonalites, and plagiogranites) and associating gabbro-anorthosites of this massif formed in the interval 576-546 Ma (U-Th-Pb zircon SHRIMP-II analysis) at the final Neoproterozoic evolution stage of the active continental margin of the Siberian craton. Our results point to a genetic relationship between the adakites and the host Nb-enriched metabasites of the Zimoveinyi massif. The studied late Neoproterozoic adakites might have formed in the setting of transform strike-slip of lithospheric plates during a halt in subduction from both crustal and mantle-crustal source, similarly to Cenozoic igneous complexes of the transform margin in the eastern framing of Eurasia.

AB - Based on new geological, structural, mineralogical, geochemical, and isotope (Sm-Nd, Rb-Sr, and U-Th-Pb) data for igneous intrusions and metamorphic rocks of the Zimoveinyi massif, an adakite-gabbroid association was identified for the first time in the Yenisei Ridge (southwestern framing of the Siberian craton). This study demonstrates that the adakites (quartz diorites, tonalites, and plagiogranites) and associating gabbro-anorthosites of this massif formed in the interval 576-546 Ma (U-Th-Pb zircon SHRIMP-II analysis) at the final Neoproterozoic evolution stage of the active continental margin of the Siberian craton. Our results point to a genetic relationship between the adakites and the host Nb-enriched metabasites of the Zimoveinyi massif. The studied late Neoproterozoic adakites might have formed in the setting of transform strike-slip of lithospheric plates during a halt in subduction from both crustal and mantle-crustal source, similarly to Cenozoic igneous complexes of the transform margin in the eastern framing of Eurasia.

KW - active and transform continental margin

KW - adakites

KW - gabbro-anorthosites

KW - late Neoproterozoic

KW - Nb-enriched metabasites

KW - Rb-Sr isotope data

KW - Siberian craton

KW - Sm-Nd

KW - U-Th-Pb

KW - Yenisei Ridge

KW - NB-ENRICHED BASALTS

KW - EVENTS

KW - ALKALINE MAGMATISM

KW - SUBDUCTION

KW - WESTERN MARGIN

KW - NOMENCLATURE

KW - EVOLUTION

KW - CRATON

KW - GEOCHEMISTRY

KW - PALEOMAGNETIC DATA

UR - http://www.scopus.com/inward/record.url?scp=85058845564&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.12.008

DO - 10.1016/j.rgg.2016.12.008

M3 - Article

AN - SCOPUS:85058845564

VL - 58

SP - 1154

EP - 1170

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 10

ER -

ID: 18292261