EARTH SURFACE DEFORMATION OF THE SAKHALIN ISLAND FROM GPS DATA
The earth surface deformation was modeled for the North, Central and South Sakhalin on the basis of de‐ formation velocities recorded by the GPS stations of the Sakhalin Geodynamical Network. A pattern of contemporary horizontal deformation is intricate in the vicinity of the main submeridional faul...
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Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2018
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ftdoajarticles:oai:doaj.org/article:34a52355102149b088f07c18c76b419a 2023-05-15T18:08:41+02:00 EARTH SURFACE DEFORMATION OF THE SAKHALIN ISLAND FROM GPS DATA A. S. Prytkov N. F. Vasilenko 2018-07-01T00:00:00Z https://doi.org/10.5800/GT-2018-9-2-0358 https://doaj.org/article/34a52355102149b088f07c18c76b419a EN RU eng rus Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust https://www.gt-crust.ru/jour/article/view/588 https://doaj.org/toc/2078-502X 2078-502X doi:10.5800/GT-2018-9-2-0358 https://doaj.org/article/34a52355102149b088f07c18c76b419a Геодинамика и тектонофизика, Vol 9, Iss 2, Pp 503-514 (2018) contemporary crustal movement gps observations deformation sakhalin island Science Q article 2018 ftdoajarticles https://doi.org/10.5800/GT-2018-9-2-0358 2022-12-30T23:02:19Z The earth surface deformation was modeled for the North, Central and South Sakhalin on the basis of de‐ formation velocities recorded by the GPS stations of the Sakhalin Geodynamical Network. A pattern of contemporary horizontal deformation is intricate in the vicinity of the main submeridional faults of the island. On the island surface, the dominant deformation regime is compression; however, the spatial distribution of deformation is heterogeneous. The horizontal compression is mainly sublatitudinal and SW‐NE‐trending. In addition to compression, there are zones of rather intense right‐lateral strike‐slip in the northern and central parts of the island, while stretching dominates in the south‐eastern parts. The regional geodynamic setting is reflected in the seismicity of the island. Recently, the seismic activity has been increased in the areas characterized by intensive surface deformation, while the areas of low deformation rates correlate with the zones of weak and sparse seismicity. Article in Journal/Newspaper Sakhalin Directory of Open Access Journals: DOAJ Articles Geodynamics & Tectonophysics 9 2 503 514 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English Russian |
topic |
contemporary crustal movement gps observations deformation sakhalin island Science Q |
spellingShingle |
contemporary crustal movement gps observations deformation sakhalin island Science Q A. S. Prytkov N. F. Vasilenko EARTH SURFACE DEFORMATION OF THE SAKHALIN ISLAND FROM GPS DATA |
topic_facet |
contemporary crustal movement gps observations deformation sakhalin island Science Q |
description |
The earth surface deformation was modeled for the North, Central and South Sakhalin on the basis of de‐ formation velocities recorded by the GPS stations of the Sakhalin Geodynamical Network. A pattern of contemporary horizontal deformation is intricate in the vicinity of the main submeridional faults of the island. On the island surface, the dominant deformation regime is compression; however, the spatial distribution of deformation is heterogeneous. The horizontal compression is mainly sublatitudinal and SW‐NE‐trending. In addition to compression, there are zones of rather intense right‐lateral strike‐slip in the northern and central parts of the island, while stretching dominates in the south‐eastern parts. The regional geodynamic setting is reflected in the seismicity of the island. Recently, the seismic activity has been increased in the areas characterized by intensive surface deformation, while the areas of low deformation rates correlate with the zones of weak and sparse seismicity. |
format |
Article in Journal/Newspaper |
author |
A. S. Prytkov N. F. Vasilenko |
author_facet |
A. S. Prytkov N. F. Vasilenko |
author_sort |
A. S. Prytkov |
title |
EARTH SURFACE DEFORMATION OF THE SAKHALIN ISLAND FROM GPS DATA |
title_short |
EARTH SURFACE DEFORMATION OF THE SAKHALIN ISLAND FROM GPS DATA |
title_full |
EARTH SURFACE DEFORMATION OF THE SAKHALIN ISLAND FROM GPS DATA |
title_fullStr |
EARTH SURFACE DEFORMATION OF THE SAKHALIN ISLAND FROM GPS DATA |
title_full_unstemmed |
EARTH SURFACE DEFORMATION OF THE SAKHALIN ISLAND FROM GPS DATA |
title_sort |
earth surface deformation of the sakhalin island from gps data |
publisher |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust |
publishDate |
2018 |
url |
https://doi.org/10.5800/GT-2018-9-2-0358 https://doaj.org/article/34a52355102149b088f07c18c76b419a |
genre |
Sakhalin |
genre_facet |
Sakhalin |
op_source |
Геодинамика и тектонофизика, Vol 9, Iss 2, Pp 503-514 (2018) |
op_relation |
https://www.gt-crust.ru/jour/article/view/588 https://doaj.org/toc/2078-502X 2078-502X doi:10.5800/GT-2018-9-2-0358 https://doaj.org/article/34a52355102149b088f07c18c76b419a |
op_doi |
https://doi.org/10.5800/GT-2018-9-2-0358 |
container_title |
Geodynamics & Tectonophysics |
container_volume |
9 |
container_issue |
2 |
container_start_page |
503 |
op_container_end_page |
514 |
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1766181003443830784 |