Application of the Controlled Source Radiomagnetotellurics (CSRMT) in the Study of Rocks Overlying Kimberlite Pipes in Yakutia/Siberia

Тhe task of searching for kimberlite pipes in covered areas of the Yakutia kimberlite province is very difficult due to the significant heterogeneity of the rocks overlying kimberlite pipes. The overlying strata of terrigenous sediments contain rocks of the trap complex (dolerite sills, tuff bodies)...

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Published in:Geosciences
Main Authors: Alexander K. Saraev, Arseny A. Shlykov, Buelent Tezkan
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
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Online Access:https://doi.org/10.3390/geosciences12010034
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author Alexander K. Saraev
Arseny A. Shlykov
Buelent Tezkan
author_facet Alexander K. Saraev
Arseny A. Shlykov
Buelent Tezkan
author_sort Alexander K. Saraev
collection MDPI Open Access Publishing
container_issue 1
container_start_page 34
container_title Geosciences
container_volume 12
description Тhe task of searching for kimberlite pipes in covered areas of the Yakutia kimberlite province is very difficult due to the significant heterogeneity of the rocks overlying kimberlite pipes. The overlying strata of terrigenous sediments contain rocks of the trap complex (dolerite sills, tuff bodies). We consider the results of the controlled source radiomagnetotelluric (CSRMT) soundings in Yakutia/Siberia. Due to the great thickness of the overlying rocks (near 100 m) and the relatively small horizontal sizes of kimberlite pipes (80–200 m), they cannot confidently be detected directly. An additional difficulty in identifying pipe anomalies is the presence of a layer of conductive carbonaceous siltstones in the overlying strata. Therefore, the main aim of the CSRMT surveys was the study of overlying rocks and the search for indirect indications of the presence of pipes. Possibilities to study the structure of dolerite sills located within overlying sediments and to map the top edge of hosting carbonate rocks are demonstrated using the CSRMT data. The pinching out of dolerite sills above pipes («windows in traps») and the lowering of the top edge of hosting rocks at pipes can be considered as indirect indications of the presence of pipes.
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genre Yakutia
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Siberia
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op_source Geosciences; Volume 12; Issue 1; Pages: 34
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spelling ftmdpi:oai:mdpi.com:/2076-3263/12/1/34/ 2025-01-17T01:18:45+00:00 Application of the Controlled Source Radiomagnetotellurics (CSRMT) in the Study of Rocks Overlying Kimberlite Pipes in Yakutia/Siberia Alexander K. Saraev Arseny A. Shlykov Buelent Tezkan agris 2022-01-12 application/pdf https://doi.org/10.3390/geosciences12010034 EN eng Multidisciplinary Digital Publishing Institute Geophysics https://dx.doi.org/10.3390/geosciences12010034 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 12; Issue 1; Pages: 34 kimberlite overlying rock controlled source radiomagnetotelluric indirect indication Text 2022 ftmdpi https://doi.org/10.3390/geosciences12010034 2023-08-01T03:48:38Z Тhe task of searching for kimberlite pipes in covered areas of the Yakutia kimberlite province is very difficult due to the significant heterogeneity of the rocks overlying kimberlite pipes. The overlying strata of terrigenous sediments contain rocks of the trap complex (dolerite sills, tuff bodies). We consider the results of the controlled source radiomagnetotelluric (CSRMT) soundings in Yakutia/Siberia. Due to the great thickness of the overlying rocks (near 100 m) and the relatively small horizontal sizes of kimberlite pipes (80–200 m), they cannot confidently be detected directly. An additional difficulty in identifying pipe anomalies is the presence of a layer of conductive carbonaceous siltstones in the overlying strata. Therefore, the main aim of the CSRMT surveys was the study of overlying rocks and the search for indirect indications of the presence of pipes. Possibilities to study the structure of dolerite sills located within overlying sediments and to map the top edge of hosting carbonate rocks are demonstrated using the CSRMT data. The pinching out of dolerite sills above pipes («windows in traps») and the lowering of the top edge of hosting rocks at pipes can be considered as indirect indications of the presence of pipes. Text Yakutia Siberia MDPI Open Access Publishing Geosciences 12 1 34
spellingShingle kimberlite
overlying rock
controlled source radiomagnetotelluric
indirect indication
Alexander K. Saraev
Arseny A. Shlykov
Buelent Tezkan
Application of the Controlled Source Radiomagnetotellurics (CSRMT) in the Study of Rocks Overlying Kimberlite Pipes in Yakutia/Siberia
title Application of the Controlled Source Radiomagnetotellurics (CSRMT) in the Study of Rocks Overlying Kimberlite Pipes in Yakutia/Siberia
title_full Application of the Controlled Source Radiomagnetotellurics (CSRMT) in the Study of Rocks Overlying Kimberlite Pipes in Yakutia/Siberia
title_fullStr Application of the Controlled Source Radiomagnetotellurics (CSRMT) in the Study of Rocks Overlying Kimberlite Pipes in Yakutia/Siberia
title_full_unstemmed Application of the Controlled Source Radiomagnetotellurics (CSRMT) in the Study of Rocks Overlying Kimberlite Pipes in Yakutia/Siberia
title_short Application of the Controlled Source Radiomagnetotellurics (CSRMT) in the Study of Rocks Overlying Kimberlite Pipes in Yakutia/Siberia
title_sort application of the controlled source radiomagnetotellurics (csrmt) in the study of rocks overlying kimberlite pipes in yakutia/siberia
topic kimberlite
overlying rock
controlled source radiomagnetotelluric
indirect indication
topic_facet kimberlite
overlying rock
controlled source radiomagnetotelluric
indirect indication
url https://doi.org/10.3390/geosciences12010034