SEQUENCE OF AILLIKITE AND CALCITE CARBONATITE FORMATION WITHIN THE BELAYA ZIMA MASSIF, EAST SIBERIA, RUSSIA

The mineralogical and geochemical features, as well as the sequence of formation of aillikite and calcite carbonatite (CC) with pyrochlore are described for the massif of alkaline ultramafic carbonatite complexes Belaya Zima located in East Siberia. Until now, mutually exclusive information presents...

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Main Authors: S. M. Zhmodik, I. V. Ashchepkov, D. K. Belyanin, E. V. Ayriyants, O. N. Kiseleva, V. A. Ponomarchuk
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2022-10-01
Series:Геодинамика и тектонофизика
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Online Access:https://www.gt-crust.ru/jour/article/view/1549
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author S. M. Zhmodik
I. V. Ashchepkov
D. K. Belyanin
E. V. Ayriyants
O. N. Kiseleva
V. A. Ponomarchuk
author_facet S. M. Zhmodik
I. V. Ashchepkov
D. K. Belyanin
E. V. Ayriyants
O. N. Kiseleva
V. A. Ponomarchuk
author_sort S. M. Zhmodik
collection DOAJ
description The mineralogical and geochemical features, as well as the sequence of formation of aillikite and calcite carbonatite (CC) with pyrochlore are described for the massif of alkaline ultramafic carbonatite complexes Belaya Zima located in East Siberia. Until now, mutually exclusive information presents the temporal relationships of carbonatites and lamprophyres of the Belaya Zima massif.The sample marking the contact of aillikite and CC was comprehensive studied using analytical methods, e.g. XRF (ARL-9900XP spectrometer, ThermoFisher Scientific), ICP-MS (Element Finnigan MAT), SEM (MIRA 3 LMU (Tescan Ltd)), transmission and ore microscopy (AxioScope. A1, Zeiss), 40Ar/39Ar age determination of micas (Argus mass spectrometer, Micromass). The data obtained indicate a later formation of CC relative to aillikites and probable separation of the carbonatite melt from a single picrite-carbonatite source.
format Article
id doaj-art-8d37c935a1b64ac0810930db054d74ea
institution Kabale University
issn 2078-502X
language English
publishDate 2022-10-01
publisher Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
record_format Article
series Геодинамика и тектонофизика
spelling doaj-art-8d37c935a1b64ac0810930db054d74ea2025-08-20T03:59:45ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2022-10-0113410.5800/GT-2022-13-4-0654654SEQUENCE OF AILLIKITE AND CALCITE CARBONATITE FORMATION WITHIN THE BELAYA ZIMA MASSIF, EAST SIBERIA, RUSSIAS. M. Zhmodik0I. V. Ashchepkov1D. K. Belyanin2E. V. Ayriyants3O. N. Kiseleva4V. A. Ponomarchuk5Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesThe mineralogical and geochemical features, as well as the sequence of formation of aillikite and calcite carbonatite (CC) with pyrochlore are described for the massif of alkaline ultramafic carbonatite complexes Belaya Zima located in East Siberia. Until now, mutually exclusive information presents the temporal relationships of carbonatites and lamprophyres of the Belaya Zima massif.The sample marking the contact of aillikite and CC was comprehensive studied using analytical methods, e.g. XRF (ARL-9900XP spectrometer, ThermoFisher Scientific), ICP-MS (Element Finnigan MAT), SEM (MIRA 3 LMU (Tescan Ltd)), transmission and ore microscopy (AxioScope. A1, Zeiss), 40Ar/39Ar age determination of micas (Argus mass spectrometer, Micromass). The data obtained indicate a later formation of CC relative to aillikites and probable separation of the carbonatite melt from a single picrite-carbonatite source.https://www.gt-crust.ru/jour/article/view/1549lamprophyrecarbonatiteaillikitemineralogygeochemistrybelaya zima massif
spellingShingle S. M. Zhmodik
I. V. Ashchepkov
D. K. Belyanin
E. V. Ayriyants
O. N. Kiseleva
V. A. Ponomarchuk
SEQUENCE OF AILLIKITE AND CALCITE CARBONATITE FORMATION WITHIN THE BELAYA ZIMA MASSIF, EAST SIBERIA, RUSSIA
Геодинамика и тектонофизика
lamprophyre
carbonatite
aillikite
mineralogy
geochemistry
belaya zima massif
title SEQUENCE OF AILLIKITE AND CALCITE CARBONATITE FORMATION WITHIN THE BELAYA ZIMA MASSIF, EAST SIBERIA, RUSSIA
title_full SEQUENCE OF AILLIKITE AND CALCITE CARBONATITE FORMATION WITHIN THE BELAYA ZIMA MASSIF, EAST SIBERIA, RUSSIA
title_fullStr SEQUENCE OF AILLIKITE AND CALCITE CARBONATITE FORMATION WITHIN THE BELAYA ZIMA MASSIF, EAST SIBERIA, RUSSIA
title_full_unstemmed SEQUENCE OF AILLIKITE AND CALCITE CARBONATITE FORMATION WITHIN THE BELAYA ZIMA MASSIF, EAST SIBERIA, RUSSIA
title_short SEQUENCE OF AILLIKITE AND CALCITE CARBONATITE FORMATION WITHIN THE BELAYA ZIMA MASSIF, EAST SIBERIA, RUSSIA
title_sort sequence of aillikite and calcite carbonatite formation within the belaya zima massif east siberia russia
topic lamprophyre
carbonatite
aillikite
mineralogy
geochemistry
belaya zima massif
url https://www.gt-crust.ru/jour/article/view/1549
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