Characterization of amphiboles from the Kola super-deep borehole, Russia by Raman and infrared spectroscopy

We present here for the first time, the Raman and infrared spectroscopic investigation of amphiboles from the World's deepest borehole, the Kola super-deep borehole, at the depth of 11.66 km. The Kola Super-deep borehole (SG-3) (henceforth referred as KSDB) is located in the northwest of the Ko...

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Published in:Geoscience Frontiers
Main Authors: Bhaskar J. Saikia, G. Parthasarathy, Felix F. Gorbatsevich, Rashmi R. Borah
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2021
Subjects:
Online Access:https://doi.org/10.1016/j.gsf.2020.12.013
https://doaj.org/article/3d65f01bfdbb477f93fb1ca1d504ca1c
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spelling ftdoajarticles:oai:doaj.org/article:3d65f01bfdbb477f93fb1ca1d504ca1c 2023-10-01T03:57:12+02:00 Characterization of amphiboles from the Kola super-deep borehole, Russia by Raman and infrared spectroscopy Bhaskar J. Saikia G. Parthasarathy Felix F. Gorbatsevich Rashmi R. Borah 2021-07-01T00:00:00Z https://doi.org/10.1016/j.gsf.2020.12.013 https://doaj.org/article/3d65f01bfdbb477f93fb1ca1d504ca1c EN eng Elsevier http://www.sciencedirect.com/science/article/pii/S1674987120302747 https://doaj.org/toc/1674-9871 1674-9871 doi:10.1016/j.gsf.2020.12.013 https://doaj.org/article/3d65f01bfdbb477f93fb1ca1d504ca1c Geoscience Frontiers, Vol 12, Iss 4, Pp 101134- (2021) Kola super-deep borehole Amphiboles Raman Infrared Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.1016/j.gsf.2020.12.013 2023-09-03T00:38:39Z We present here for the first time, the Raman and infrared spectroscopic investigation of amphiboles from the World's deepest borehole, the Kola super-deep borehole, at the depth of 11.66 km. The Kola Super-deep borehole (SG-3) (henceforth referred as KSDB) is located in the northwest of the Kola Peninsula in the northern frame of the Pechenga structure, Russia. It was drilled in the north-eastern part of the Baltic Shield (69о5’N, 30о44’E) and reached a depth of 12.262 km. It has been drilled in the northern limb of the Pechenga geosyncline composed of rhythmically inter-bedded volcanogenic and tuffaceous-sedimentary strata extending to the NW at 300°–310° and dipping to SW at angles of 30°–50°. The SG-3 geological section is represented by two complexes – Proterozoic and Archaean. Amphibolite facies is dominant in the depth region from 6000 m to 12,000 m to the deepest.The Raman spectra of the sample reveal abundant presence of plagioclase and amphiboles. The most distinct Raman peak in this study indicates the tremolite-ferro-actinolite rich enrichment of the borehole samples at this depth corroborating earlier conventional petrographic studies. Article in Journal/Newspaper kola peninsula Directory of Open Access Journals: DOAJ Articles Ferro ENVELOPE(16.233,16.233,66.717,66.717) Kola Peninsula Pechenga ENVELOPE(30.989,30.989,69.401,69.401) Geoscience Frontiers 12 4 101134
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Kola super-deep borehole
Amphiboles
Raman
Infrared
Geology
QE1-996.5
spellingShingle Kola super-deep borehole
Amphiboles
Raman
Infrared
Geology
QE1-996.5
Bhaskar J. Saikia
G. Parthasarathy
Felix F. Gorbatsevich
Rashmi R. Borah
Characterization of amphiboles from the Kola super-deep borehole, Russia by Raman and infrared spectroscopy
topic_facet Kola super-deep borehole
Amphiboles
Raman
Infrared
Geology
QE1-996.5
description We present here for the first time, the Raman and infrared spectroscopic investigation of amphiboles from the World's deepest borehole, the Kola super-deep borehole, at the depth of 11.66 km. The Kola Super-deep borehole (SG-3) (henceforth referred as KSDB) is located in the northwest of the Kola Peninsula in the northern frame of the Pechenga structure, Russia. It was drilled in the north-eastern part of the Baltic Shield (69о5’N, 30о44’E) and reached a depth of 12.262 km. It has been drilled in the northern limb of the Pechenga geosyncline composed of rhythmically inter-bedded volcanogenic and tuffaceous-sedimentary strata extending to the NW at 300°–310° and dipping to SW at angles of 30°–50°. The SG-3 geological section is represented by two complexes – Proterozoic and Archaean. Amphibolite facies is dominant in the depth region from 6000 m to 12,000 m to the deepest.The Raman spectra of the sample reveal abundant presence of plagioclase and amphiboles. The most distinct Raman peak in this study indicates the tremolite-ferro-actinolite rich enrichment of the borehole samples at this depth corroborating earlier conventional petrographic studies.
format Article in Journal/Newspaper
author Bhaskar J. Saikia
G. Parthasarathy
Felix F. Gorbatsevich
Rashmi R. Borah
author_facet Bhaskar J. Saikia
G. Parthasarathy
Felix F. Gorbatsevich
Rashmi R. Borah
author_sort Bhaskar J. Saikia
title Characterization of amphiboles from the Kola super-deep borehole, Russia by Raman and infrared spectroscopy
title_short Characterization of amphiboles from the Kola super-deep borehole, Russia by Raman and infrared spectroscopy
title_full Characterization of amphiboles from the Kola super-deep borehole, Russia by Raman and infrared spectroscopy
title_fullStr Characterization of amphiboles from the Kola super-deep borehole, Russia by Raman and infrared spectroscopy
title_full_unstemmed Characterization of amphiboles from the Kola super-deep borehole, Russia by Raman and infrared spectroscopy
title_sort characterization of amphiboles from the kola super-deep borehole, russia by raman and infrared spectroscopy
publisher Elsevier
publishDate 2021
url https://doi.org/10.1016/j.gsf.2020.12.013
https://doaj.org/article/3d65f01bfdbb477f93fb1ca1d504ca1c
long_lat ENVELOPE(16.233,16.233,66.717,66.717)
ENVELOPE(30.989,30.989,69.401,69.401)
geographic Ferro
Kola Peninsula
Pechenga
geographic_facet Ferro
Kola Peninsula
Pechenga
genre kola peninsula
genre_facet kola peninsula
op_source Geoscience Frontiers, Vol 12, Iss 4, Pp 101134- (2021)
op_relation http://www.sciencedirect.com/science/article/pii/S1674987120302747
https://doaj.org/toc/1674-9871
1674-9871
doi:10.1016/j.gsf.2020.12.013
https://doaj.org/article/3d65f01bfdbb477f93fb1ca1d504ca1c
op_doi https://doi.org/10.1016/j.gsf.2020.12.013
container_title Geoscience Frontiers
container_volume 12
container_issue 4
container_start_page 101134
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