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

S. Zhmodik; P. Ivanov; D. Belyanin; E. Airiyants; O. Kiseleva; A. Travin

doi:10.1088/1755-1315/319/1/012023

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

S. Zhmodik, P. Ivanov, D. Belyanin, E. Airiyants, O. Kiseleva, A. Travin

Research output: Contribution to journal › Conference article › peer-review

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.

Original language	English
Article number	012023
Number of pages	16
Journal	IOP Conference Series: Earth and Environmental Science
Volume	319
Issue number	1
DOIs	https://doi.org/10.1088/1755-1315/319/1/012023
Publication status	Published - 19 Sep 2019
Event	10th All Russian Petrographic Conference with International Participationon Petrology of Magnetic and Metamorphic Complexes - Tomsk, Russian Federation Duration: 27 Nov 2018 → 28 Nov 2018

Keywords

TUFFISITIC KIMBERLITE
IMPACT STRUCTURE
POPIGAI
EVENTS
ROCKS

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10.1088/1755-1315/319/1/012023

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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.",

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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.

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KW - POPIGAI

KW - EVENTS

KW - ROCKS

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