V. I. Kaftan, I. K. Mironov, A. I. Manevich, R. V. Shvchuk, V. M. Maguskin
{"title":"2015 - 2023年堪察加半岛阿瓦恰火山地区地壳近期运动与变形","authors":"V. I. Kaftan, I. K. Mironov, A. I. Manevich, R. V. Shvchuk, V. M. Maguskin","doi":"10.1134/S1069351325700302","DOIUrl":null,"url":null,"abstract":"<p>The article presents the results of studies of modern movements and deformations according to GNSS observations in the area of Avacha volcano in 2015–2023. Studies of Avacha volcano are particularly important, because it is an active volcano closest to the administrative center of Kamchatka Krai. Interesting features of the local geodynamics of the area were revealed. Horizontal and vertical displacements, dilatation, and full shear deformations, as well as characteristics of the deficit of “internal” displacements were analyzed. In the southern part of the network, there is an accumulation of compression deformation due to pressure from the subduction zone. In the vicinity of the volcanic crater, tensile strain accumulates in the absence of significant uplift. The characteristics of the internal displacement deficit show the response of the GNSS network to the <i>M</i>6.5 earthquake (April 3, 2023) All changes in the characteristics of crustal motions and deformations demonstrated about a 2-year cyclicity. In further observations it will be possible to evaluate the stability of this phenomenon. Also noteworthy is the need to expand the GNSS observation network to the northern slope and foot of Avacha volcano for more detailed geodetic monitoring of its state.</p>","PeriodicalId":602,"journal":{"name":"Izvestiya, Physics of the Solid Earth","volume":"61 3","pages":"385 - 395"},"PeriodicalIF":1.0000,"publicationDate":"2025-08-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Recent Movements and Deformations of the Earth’s Crust in the Region of Avacha Volcano (Kamchatka Peninsula) from 2015 to 2023\",\"authors\":\"V. I. Kaftan, I. K. Mironov, A. I. Manevich, R. V. Shvchuk, V. M. Maguskin\",\"doi\":\"10.1134/S1069351325700302\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>The article presents the results of studies of modern movements and deformations according to GNSS observations in the area of Avacha volcano in 2015–2023. Studies of Avacha volcano are particularly important, because it is an active volcano closest to the administrative center of Kamchatka Krai. Interesting features of the local geodynamics of the area were revealed. Horizontal and vertical displacements, dilatation, and full shear deformations, as well as characteristics of the deficit of “internal” displacements were analyzed. In the southern part of the network, there is an accumulation of compression deformation due to pressure from the subduction zone. In the vicinity of the volcanic crater, tensile strain accumulates in the absence of significant uplift. The characteristics of the internal displacement deficit show the response of the GNSS network to the <i>M</i>6.5 earthquake (April 3, 2023) All changes in the characteristics of crustal motions and deformations demonstrated about a 2-year cyclicity. In further observations it will be possible to evaluate the stability of this phenomenon. Also noteworthy is the need to expand the GNSS observation network to the northern slope and foot of Avacha volcano for more detailed geodetic monitoring of its state.</p>\",\"PeriodicalId\":602,\"journal\":{\"name\":\"Izvestiya, Physics of the Solid Earth\",\"volume\":\"61 3\",\"pages\":\"385 - 395\"},\"PeriodicalIF\":1.0000,\"publicationDate\":\"2025-08-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Izvestiya, Physics of the Solid Earth\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1134/S1069351325700302\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Izvestiya, Physics of the Solid Earth","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1134/S1069351325700302","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Recent Movements and Deformations of the Earth’s Crust in the Region of Avacha Volcano (Kamchatka Peninsula) from 2015 to 2023
The article presents the results of studies of modern movements and deformations according to GNSS observations in the area of Avacha volcano in 2015–2023. Studies of Avacha volcano are particularly important, because it is an active volcano closest to the administrative center of Kamchatka Krai. Interesting features of the local geodynamics of the area were revealed. Horizontal and vertical displacements, dilatation, and full shear deformations, as well as characteristics of the deficit of “internal” displacements were analyzed. In the southern part of the network, there is an accumulation of compression deformation due to pressure from the subduction zone. In the vicinity of the volcanic crater, tensile strain accumulates in the absence of significant uplift. The characteristics of the internal displacement deficit show the response of the GNSS network to the M6.5 earthquake (April 3, 2023) All changes in the characteristics of crustal motions and deformations demonstrated about a 2-year cyclicity. In further observations it will be possible to evaluate the stability of this phenomenon. Also noteworthy is the need to expand the GNSS observation network to the northern slope and foot of Avacha volcano for more detailed geodetic monitoring of its state.
期刊介绍:
Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.