RECONSTRUCTION OF THE DEEP STRUCTURE OF THE WEST SPITSBERGEN ISLAND AREA BASED ON THE RESULTS OF XENOLITE STUDIES IN QUATERNARY VOLCANOES
A brief petrographic characterization of rocks of the area of manifestation of Quaternary volcanism on the island of West Svalbard is given, as well as the composition of deep xenoliths from the volcanic buildings Sverrefjellet, Halvdanpiggen and Sigurdfjellet. Peridotite and pyroxenite geotherms fo...
Main Authors: | , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Zenodo
2023
|
Subjects: | |
Online Access: | https://doi.org/10.5281/zenodo.7513809 |
id |
ftzenodo:oai:zenodo.org:7513809 |
---|---|
record_format |
openpolar |
spelling |
ftzenodo:oai:zenodo.org:7513809 2024-09-15T18:38:16+00:00 RECONSTRUCTION OF THE DEEP STRUCTURE OF THE WEST SPITSBERGEN ISLAND AREA BASED ON THE RESULTS OF XENOLITE STUDIES IN QUATERNARY VOLCANOES Evdokimov A. Kireev V. 2023-01-08 https://doi.org/10.5281/zenodo.7513809 unknown Zenodo https://doi.org/10.5281/zenodo.7513808 https://doi.org/10.5281/zenodo.7513809 oai:zenodo.org:7513809 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode The scientific heritage, 104, 33-42, (2023-01-08) West Svalbard deep xenoliths thermobarometry crustal thickness info:eu-repo/semantics/article 2023 ftzenodo https://doi.org/10.5281/zenodo.751380910.5281/zenodo.7513808 2024-07-27T06:05:32Z A brief petrographic characterization of rocks of the area of manifestation of Quaternary volcanism on the island of West Svalbard is given, as well as the composition of deep xenoliths from the volcanic buildings Sverrefjellet, Halvdanpiggen and Sigurdfjellet. Peridotite and pyroxenite geotherms for the period of formation of the lower crust and upper mantle have been determined according to the data of temperature and pressure determination during crystallization of deep xenoliths. Comparison with modern geophysical data on the deep structure of the archipelago region, reconstruction of the depths of the formation of peridotites and pyroxenites in the Grenville era of tectonic-magmatic events allows us to conclude that the thickness of the modern Earth's crust in the area of West Svalbard island is reduced by almost 16 km over a period of almost 900 million years. Obviously, this process could occur due to the expansion of the volume of the planet or The Earth crust spreading. Article in Journal/Newspaper Svalbard Spitsbergen Zenodo |
institution |
Open Polar |
collection |
Zenodo |
op_collection_id |
ftzenodo |
language |
unknown |
topic |
West Svalbard deep xenoliths thermobarometry crustal thickness |
spellingShingle |
West Svalbard deep xenoliths thermobarometry crustal thickness Evdokimov A. Kireev V. RECONSTRUCTION OF THE DEEP STRUCTURE OF THE WEST SPITSBERGEN ISLAND AREA BASED ON THE RESULTS OF XENOLITE STUDIES IN QUATERNARY VOLCANOES |
topic_facet |
West Svalbard deep xenoliths thermobarometry crustal thickness |
description |
A brief petrographic characterization of rocks of the area of manifestation of Quaternary volcanism on the island of West Svalbard is given, as well as the composition of deep xenoliths from the volcanic buildings Sverrefjellet, Halvdanpiggen and Sigurdfjellet. Peridotite and pyroxenite geotherms for the period of formation of the lower crust and upper mantle have been determined according to the data of temperature and pressure determination during crystallization of deep xenoliths. Comparison with modern geophysical data on the deep structure of the archipelago region, reconstruction of the depths of the formation of peridotites and pyroxenites in the Grenville era of tectonic-magmatic events allows us to conclude that the thickness of the modern Earth's crust in the area of West Svalbard island is reduced by almost 16 km over a period of almost 900 million years. Obviously, this process could occur due to the expansion of the volume of the planet or The Earth crust spreading. |
format |
Article in Journal/Newspaper |
author |
Evdokimov A. Kireev V. |
author_facet |
Evdokimov A. Kireev V. |
author_sort |
Evdokimov A. |
title |
RECONSTRUCTION OF THE DEEP STRUCTURE OF THE WEST SPITSBERGEN ISLAND AREA BASED ON THE RESULTS OF XENOLITE STUDIES IN QUATERNARY VOLCANOES |
title_short |
RECONSTRUCTION OF THE DEEP STRUCTURE OF THE WEST SPITSBERGEN ISLAND AREA BASED ON THE RESULTS OF XENOLITE STUDIES IN QUATERNARY VOLCANOES |
title_full |
RECONSTRUCTION OF THE DEEP STRUCTURE OF THE WEST SPITSBERGEN ISLAND AREA BASED ON THE RESULTS OF XENOLITE STUDIES IN QUATERNARY VOLCANOES |
title_fullStr |
RECONSTRUCTION OF THE DEEP STRUCTURE OF THE WEST SPITSBERGEN ISLAND AREA BASED ON THE RESULTS OF XENOLITE STUDIES IN QUATERNARY VOLCANOES |
title_full_unstemmed |
RECONSTRUCTION OF THE DEEP STRUCTURE OF THE WEST SPITSBERGEN ISLAND AREA BASED ON THE RESULTS OF XENOLITE STUDIES IN QUATERNARY VOLCANOES |
title_sort |
reconstruction of the deep structure of the west spitsbergen island area based on the results of xenolite studies in quaternary volcanoes |
publisher |
Zenodo |
publishDate |
2023 |
url |
https://doi.org/10.5281/zenodo.7513809 |
genre |
Svalbard Spitsbergen |
genre_facet |
Svalbard Spitsbergen |
op_source |
The scientific heritage, 104, 33-42, (2023-01-08) |
op_relation |
https://doi.org/10.5281/zenodo.7513808 https://doi.org/10.5281/zenodo.7513809 oai:zenodo.org:7513809 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.751380910.5281/zenodo.7513808 |
_version_ |
1810482591773491200 |