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40Ar/39Ar geochronology of alkaline rocks of the Inagli Massif (Aldan Shield, southern Yakutia). / Ponomarchuk, A.; Prokop'ev, I. R.; Svetlitskaya, T. V. et al.

In: Russian Geology and Geophysics, Vol. 60, No. 1, 01.01.2019, p. 33-44.

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

Harvard

Ponomarchuk, A, Prokop'ev, IR, Svetlitskaya, TV & Doroshkevich, AG 2019, '40Ar/39Ar geochronology of alkaline rocks of the Inagli Massif (Aldan Shield, southern Yakutia)', Russian Geology and Geophysics, vol. 60, no. 1, pp. 33-44. https://doi.org/10.15372/RGG2019003

APA

Ponomarchuk, A., Prokop'ev, I. R., Svetlitskaya, T. V., & Doroshkevich, A. G. (2019). 40Ar/39Ar geochronology of alkaline rocks of the Inagli Massif (Aldan Shield, southern Yakutia). Russian Geology and Geophysics, 60(1), 33-44. https://doi.org/10.15372/RGG2019003

Vancouver

Ponomarchuk A, Prokop'ev IR, Svetlitskaya TV, Doroshkevich AG. 40Ar/39Ar geochronology of alkaline rocks of the Inagli Massif (Aldan Shield, southern Yakutia). Russian Geology and Geophysics. 2019 Jan 1;60(1):33-44. doi: 10.15372/RGG2019003

Author

Ponomarchuk, A. ; Prokop'ev, I. R. ; Svetlitskaya, T. V. et al. / 40Ar/39Ar geochronology of alkaline rocks of the Inagli Massif (Aldan Shield, southern Yakutia). In: Russian Geology and Geophysics. 2019 ; Vol. 60, No. 1. pp. 33-44.

BibTeX

@article{16ee6d85fed644b4bac05b0794d213cb,
title = "40Ar/39Ar geochronology of alkaline rocks of the Inagli Massif (Aldan Shield, southern Yakutia)",
abstract = "The Inagli zoned ring massif is located in the Central Aldan ore district. The close localization of ultrabasic and alkaline potassic rocks, magmatism, and mineralization (platinum, gems Cr-diopside, and vermiculite) make this object unique from both geological and economic perspectives. Formation of alkaline rocks in the Inagli massif was related to the Mesozoic tectonomagmatic activation of the Aldan Shield and occurred in several stages. Intrusion of clinopyroxenites took place no later than 145.8 +/- 3.2 Ma, whereas most of alkaline rocks of the ring framing formed at 133-128 Ma. The feldspar-Cr-diopside-mica veins in the dunite core are dated at 133.4 +/- 1 Ma.",
keywords = "Inagli massif, Ar-Ar dating, zoned ring massifs, dating of alkaline rocks, Mesozoic igneous rocks, KONDER MASSIF, AGE, MINERALIZATION, PROVINCE, SIBERIA, ORIGIN, Zoned ring massifs, Ar–Ar dating, Dating of alkaline rocks",
author = "A. Ponomarchuk and Prokop'ev, {I. R.} and Svetlitskaya, {T. V.} and Doroshkevich, {A. G.}",
year = "2019",
month = jan,
day = "1",
doi = "10.15372/RGG2019003",
language = "English",
volume = "60",
pages = "33--44",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "1",

}

RIS

TY - JOUR

T1 - 40Ar/39Ar geochronology of alkaline rocks of the Inagli Massif (Aldan Shield, southern Yakutia)

AU - Ponomarchuk, A.

AU - Prokop'ev, I. R.

AU - Svetlitskaya, T. V.

AU - Doroshkevich, A. G.

PY - 2019/1/1

Y1 - 2019/1/1

N2 - The Inagli zoned ring massif is located in the Central Aldan ore district. The close localization of ultrabasic and alkaline potassic rocks, magmatism, and mineralization (platinum, gems Cr-diopside, and vermiculite) make this object unique from both geological and economic perspectives. Formation of alkaline rocks in the Inagli massif was related to the Mesozoic tectonomagmatic activation of the Aldan Shield and occurred in several stages. Intrusion of clinopyroxenites took place no later than 145.8 +/- 3.2 Ma, whereas most of alkaline rocks of the ring framing formed at 133-128 Ma. The feldspar-Cr-diopside-mica veins in the dunite core are dated at 133.4 +/- 1 Ma.

AB - The Inagli zoned ring massif is located in the Central Aldan ore district. The close localization of ultrabasic and alkaline potassic rocks, magmatism, and mineralization (platinum, gems Cr-diopside, and vermiculite) make this object unique from both geological and economic perspectives. Formation of alkaline rocks in the Inagli massif was related to the Mesozoic tectonomagmatic activation of the Aldan Shield and occurred in several stages. Intrusion of clinopyroxenites took place no later than 145.8 +/- 3.2 Ma, whereas most of alkaline rocks of the ring framing formed at 133-128 Ma. The feldspar-Cr-diopside-mica veins in the dunite core are dated at 133.4 +/- 1 Ma.

KW - Inagli massif

KW - Ar-Ar dating

KW - zoned ring massifs

KW - dating of alkaline rocks

KW - Mesozoic igneous rocks

KW - KONDER MASSIF

KW - AGE

KW - MINERALIZATION

KW - PROVINCE

KW - SIBERIA

KW - ORIGIN

KW - Zoned ring massifs

KW - Ar–Ar dating

KW - Dating of alkaline rocks

UR - http://www.scopus.com/inward/record.url?scp=85079480156&partnerID=8YFLogxK

U2 - 10.15372/RGG2019003

DO - 10.15372/RGG2019003

M3 - Article

VL - 60

SP - 33

EP - 44

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 1

ER -

ID: 23292949