The research of interrelation between seismic activity and modern horisontal movements of the Carpathian-Balkan region based on the data from permanent GNSS stations

dc.citation.epage18
dc.citation.issue1 (28)
dc.citation.journalTitleГеодинаміка
dc.citation.spage5
dc.contributor.affiliationНаціональний університет “Львівська політехніка”
dc.contributor.affiliationLviv Polytechnic National University
dc.contributor.authorТретяк, К. Р.
dc.contributor.authorБрусак, І. В.
dc.contributor.authorTretyak, K. R.
dc.contributor.authorBrusak, I.
dc.coverage.placenameЛьвів
dc.coverage.placenameLviv
dc.date.accessioned2023-06-20T07:49:25Z
dc.date.available2023-06-20T07:49:25Z
dc.date.created2020-02-25
dc.date.issued2020-02-25
dc.description.abstractПроблема прогнозу землетрусів та їх взаємозв’язку із горизонтальними деформаціями земної кори досі не вирішена. У цій роботі метою є пошук просторово-часових взаємозв’язків між значеннями узагальнених критеріїв поля горизонтальних швидкостей земної кори та узагальненої сейсмічності. Як полігон досліджень вибрано територію Карпато-Балканського регіону, в зв’язку із широкою диференціацією сейсмічної активності та добре дослідженою геологічною структурою регіону. Методика. За даними мереж ГНСС-станцій проаналізовано горизонтальні деформації території Карпато-Балканського регіону за 2010–2019 рр. та побудовано карти розподілу швидкостей дилатації. За даними сейсмічних станцій визначено щорічні параметри узагальненої сейсмічності для окремих блоків, у вершинах яких розташовані ГНСС-станції. На основі просторово-часового аналізу горизонтальних деформацій та узагальненої сейсмічності здійснено пошук кореляційних взаємозв’язків між абсолютним значеннями дилатації та узагальненими параметрами сейсмічності територій. У результаті виділено сталі зони, із високим ступенем кореляції між абсолютним значеннями дилатації та великою піввіссю еліпса розсіювання землетрусів. Найбільша за площею територія із високою кореляцією охоплює Родопський масив, зону занурення Африканської плити під Євразійську. Територія високої кореляції також збігається із зоною Вранча. На основі виконаних досліджень можна припустити, що кореляційний взаємозв’язок між горизонтальними деформаціями, визначеними за даними ГНСС, і узагальненою сейсмічністю проявляється тільки у зонах субдукції, де є інтенсивна сейсмоактивність і прояви постійних деформацій земної кори. Це підтверджується проявом зон кореляцій, які розташовані вздовж однієї зі сторін активних розломів.
dc.description.abstractThe problem of earthquake prediction, as well as its interrelation with horizontal movements of the Earth’s crust has not still been solved. The purpose of the work is to establish a possible correlation between generalized parameters of horizontal movements of the Earth’s crust and seismicity. The Carpathian-Balkan region in connection with frequent and spatial differentiation of earthquake activity and well-known geological structures is chosen as a field for the research. Methods. Based on the data of permanent GNSS stations in 2010–2019, the horizontal velocities and deformations of the Carpathian-Balkan region are analyzed, as well as the maps of fields of the annual distribution of dilatation are added. The annual generalized parameters of seismicity for separate blocks are calculated from the data of seismological stations. Based on the spatial analysis of horizontal deformations and generalized seismicity, the correlations between absolute values of dilatation and semi-major axis of ellipse of scattering earthquake epicenters are established. As the results, the authors demonstrate some territories covered by the annual high degree of correlative connection between semi-major axis of the ellipse of scattering earthquake epicenters and absolute values of dilatation. The biggest correlative zone includes the Rhodopes, a subduction zone between Nubia and Europe tectonic units. The territory of stable correlations also coincides with Vrancea. The research suggests that the interconnection between horizontal deformations and generalized seismicity occurs only in subduction zones where there are both intense seismic activity and regular crust deformations. This is confirmed by the appearance of correlation zones which are located along one side of the active faults.
dc.format.extent5-18
dc.format.pages14
dc.identifier.citationTretyak K. R. The research of interrelation between seismic activity and modern horisontal movements of the Carpathian-Balkan region based on the data from permanent GNSS stations / K. R. Tretyak, I. Brusak // Geodynamics. — Lviv : Lviv Politechnic Publishing House, 2020. — No 1 (28). — P. 5–18.
dc.identifier.citationenTretyak K. R. The research of interrelation between seismic activity and modern horisontal movements of the Carpathian-Balkan region based on the data from permanent GNSS stations / K. R. Tretyak, I. Brusak // Geodynamics. — Lviv : Lviv Politechnic Publishing House, 2020. — No 1 (28). — P. 5–18.
dc.identifier.doidoi.org/10.23939/jgd2020.01.005
dc.identifier.urihttps://ena.lpnu.ua/handle/ntb/59287
dc.language.isoen
dc.publisherВидавництво Львівської політехніки
dc.publisherLviv Politechnic Publishing House
dc.relation.ispartofГеодинаміка, 1 (28), 2020
dc.relation.ispartofGeodynamics, 1 (28), 2020
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dc.relation.referencesen(2014). Mantle dynamics in the Mediterranean.
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dc.relation.referencesenindicator of geodynamic process. Geophisicheskiy
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dc.relation.referencesenResearch Letters, 32(16).
dc.relation.referencesenGulal, E., Tiryakioglu, I., Kalyoncuoglu, U. Y.,
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dc.relation.referencesenThe determination of relations between statistical
dc.relation.referencesenseismicity data and geodetic strain analysis, and
dc.relation.referencesenthe analysis of seismic hazard in southwest Anatolia.
dc.relation.referencesenGeomatics, Natural Hazards and Risk, 7(1), 138–155.
dc.relation.referencesenHalpaap, F., Rondenay, S., & Ottemöller, L. (2018).
dc.relation.referencesenSeismicity, deformation, and metamorphism in the
dc.relation.referencesenWestern Hellenic subduction zone: New constraints from tomography. Journal of Geophysical
dc.relation.referencesenResearch: Solid Earth, 123(4), 3000–3026.
dc.relation.referencesenHandy, M. R., Giese, J., Schmid, S. M., Pleuger, J.,
dc.relation.referencesenSpakman, W., Onuzi, K., & Ustaszewski, K. (2019).
dc.relation.referencesenCoupled Crust-Mantle Response to Slab Tearing,
dc.relation.referencesenBending, and Rollback Along the DinarideHellenide Orogen. Tectonics, 38(8), 2803–2828.
dc.relation.referencesenHollenstein, C., Müller, M. D., Geiger, A., & Kahle, H. G.
dc.relation.referencesen(2008). Crustal motion and deformation in Greece
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dc.relation.referencesentectonics in Vrancea zone (Romania) interpreted
dc.relation.referencesenon recent seismicity, geophysical and GPS data.
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dc.relation.referencesenCloetingh, S., & Panza, G. (2012). Geodynamics
dc.relation.referencesenand intermediate-depth seismicity in Vrancea (the
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dc.relation.urihttps://doi.org/10.1029/2018EO104623
dc.relation.urihttps://www.emsc-csem.org
dc.rights.holder© Інститут геології і геохімії горючих копалин Національної академії наук України, 2020
dc.rights.holder© Інститут геофізики ім. С. І. Субботіна Національної академії наук України, 2020
dc.rights.holder© Національний університет “Львівська політехніка”, 2020
dc.rights.holder© Tretyak K. R., Brusak I.
dc.subjectгоризонтальні деформації земної кори
dc.subjectперманентні ГНСС-станції
dc.subjectземлетрус
dc.subjectвзаємозв’язок сейсмічності та руху ГНСС-станцій
dc.subjecthorizontal deformations of the Earth's crust
dc.subjectpermanent GNSS stations
dc.subjectearthquakes
dc.subjectinterrelation between seismicity and movements of GNSS stations
dc.subject.udc528.22
dc.titleThe research of interrelation between seismic activity and modern horisontal movements of the Carpathian-Balkan region based on the data from permanent GNSS stations
dc.title.alternativeДослідження взаємозв’язку сейсмічності та сучасних горизонтальних зміщень за даними перманентних ГНСС-станцій у Карпато-Балканському регіоні
dc.typeArticle

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