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The glasses from Mesozoic sediments of Anabar region (Arctic Siberia, Russia). / Zhmodik, S.; Ivanov, P.; Belyanin, D. и др.

в: IOP Conference Series: Earth and Environmental Science, Том 319, № 1, 012023, 19.09.2019.

Результаты исследований: Научные публикации в периодических изданиях › статья по материалам конференции › Рецензирование

Harvard

Zhmodik, S, Ivanov, P, Belyanin, D, Airiyants, E, Kiseleva, O & Travin, A 2019, 'The glasses from Mesozoic sediments of Anabar region (Arctic Siberia, Russia)', IOP Conference Series: Earth and Environmental Science, Том. 319, № 1, 012023. https://doi.org/10.1088/1755-1315/319/1/012023

APA

Zhmodik, S., Ivanov, P., Belyanin, D., Airiyants, E., Kiseleva, O., & Travin, A. (2019). The glasses from Mesozoic sediments of Anabar region (Arctic Siberia, Russia). IOP Conference Series: Earth and Environmental Science, 319(1), [012023]. https://doi.org/10.1088/1755-1315/319/1/012023

Vancouver

Zhmodik S, Ivanov P, Belyanin D, Airiyants E, Kiseleva O, Travin A. The glasses from Mesozoic sediments of Anabar region (Arctic Siberia, Russia). IOP Conference Series: Earth and Environmental Science. 2019 сент. 19;319(1):012023. doi: 10.1088/1755-1315/319/1/012023

Author

Zhmodik, S. ; Ivanov, P. ; Belyanin, D. и др. / The glasses from Mesozoic sediments of Anabar region (Arctic Siberia, Russia). в: IOP Conference Series: Earth and Environmental Science. 2019 ; Том 319, № 1.

BibTeX

@article{a190758906aa46b999b166b5784fd2f1,
title = "The glasses from Mesozoic sediments of Anabar region (Arctic Siberia, Russia)",
abstract = "The glasses were found in the tuffisites of Orto-Yiarginskoe field (Anabar region, Arctic Siberia). The composition of the glasses is comparable with the composition of the glasses from the Popigai impact structure and the gneisses of the Archean basement of the Anabar folded system. The age of the studied glasses is comparable with the age of the glasses of the Popigai impact structure. Mineralogical studies were carried out using scanning electron microscopy (MIRA 3 LMU, Tescan Ltd) with the INCA Energy 450+ XMax 80 microanalysis system (Oxford Instruments Ltd). The age of the glasses is determined by the 40Ar-39Ar method in the Collective Use Center of the IGM SB RAS.",
keywords = "TUFFISITIC KIMBERLITE, IMPACT STRUCTURE, POPIGAI, EVENTS, ROCKS",
author = "S. Zhmodik and P. Ivanov and D. Belyanin and E. Airiyants and O. Kiseleva and A. Travin",
year = "2019",
month = sep,
day = "19",
doi = "10.1088/1755-1315/319/1/012023",
language = "English",
volume = "319",
journal = "IOP Conference Series: Earth and Environmental Science",
issn = "1755-1307",
publisher = "IOP Publishing Ltd.",
number = "1",
note = "10th All Russian Petrographic Conference with International Participationon Petrology of Magnetic and Metamorphic Complexes ; Conference date: 27-11-2018 Through 28-11-2018",

}

RIS

TY - JOUR

T1 - The glasses from Mesozoic sediments of Anabar region (Arctic Siberia, Russia)

AU - Zhmodik, S.

AU - Ivanov, P.

AU - Belyanin, D.

AU - Airiyants, E.

AU - Kiseleva, O.

AU - Travin, A.

PY - 2019/9/19

Y1 - 2019/9/19

N2 - The glasses were found in the tuffisites of Orto-Yiarginskoe field (Anabar region, Arctic Siberia). The composition of the glasses is comparable with the composition of the glasses from the Popigai impact structure and the gneisses of the Archean basement of the Anabar folded system. The age of the studied glasses is comparable with the age of the glasses of the Popigai impact structure. Mineralogical studies were carried out using scanning electron microscopy (MIRA 3 LMU, Tescan Ltd) with the INCA Energy 450+ XMax 80 microanalysis system (Oxford Instruments Ltd). The age of the glasses is determined by the 40Ar-39Ar method in the Collective Use Center of the IGM SB RAS.

AB - The glasses were found in the tuffisites of Orto-Yiarginskoe field (Anabar region, Arctic Siberia). The composition of the glasses is comparable with the composition of the glasses from the Popigai impact structure and the gneisses of the Archean basement of the Anabar folded system. The age of the studied glasses is comparable with the age of the glasses of the Popigai impact structure. Mineralogical studies were carried out using scanning electron microscopy (MIRA 3 LMU, Tescan Ltd) with the INCA Energy 450+ XMax 80 microanalysis system (Oxford Instruments Ltd). The age of the glasses is determined by the 40Ar-39Ar method in the Collective Use Center of the IGM SB RAS.

KW - TUFFISITIC KIMBERLITE

KW - IMPACT STRUCTURE

KW - POPIGAI

KW - EVENTS

KW - ROCKS

UR - http://www.scopus.com/inward/record.url?scp=85073056990&partnerID=8YFLogxK

U2 - 10.1088/1755-1315/319/1/012023

DO - 10.1088/1755-1315/319/1/012023

M3 - Conference article

AN - SCOPUS:85073056990

VL - 319

JO - IOP Conference Series: Earth and Environmental Science

JF - IOP Conference Series: Earth and Environmental Science

SN - 1755-1307

IS - 1

M1 - 012023

T2 - 10th All Russian Petrographic Conference with International Participationon Petrology of Magnetic and Metamorphic Complexes

Y2 - 27 November 2018 through 28 November 2018

ER -

ID: 21857314