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dc.contributor.author	Pihulevskyi, P. G.
dc.contributor.author	Anisimova, L. B.
dc.contributor.author	Kalinichenko, O. O.
dc.contributor.author	Panteleeva, N. B.
dc.contributor.author	Hanchuk, O. V.
dc.contributor.author	Калініченко, Ольга Олександрівна
dc.contributor.author	Пантелєєва, Наталя Борисівна
dc.contributor.author	Ганчук, Олена Вікторівна
dc.date.accessioned	2021-09-26T13:08:48Z
dc.date.available	2021-09-26T13:08:48Z
dc.date.issued	2021-03-19
dc.identifier.citation	Pihulevskyi P. G. Analysis of natural and technogenic factors on the seismicity of Kryvyi Rih / P. G. Pihulevskyi, L. B. Anisimova, O. O. Kalinichenko, N. B. Panteleeva, O. V. Hanchuk // Journal of Physics: Conference Series. - 2021. - Vol. 1840. - Article 012018. - DOI : https://doi.org/10.1088/1742-6596/1840/1/012018	uk
dc.identifier.issn	1742-6596
dc.identifier.uri	http://elibrary.kdpu.edu.ua/xmlui/handle/123456789/4561
dc.identifier.uri	https://doi.org/10.31812/123456789/4561
dc.description	[1] Andrushchenko Yu A, Kutas V V, Kendzera A V and Omelchenko V D 2012 Weak earthquakes and industrial explosions registered on the Eastern European platform within the territory of Ukraine in 2005-2010. Geofizicheskiy Zhurnal 34 49–60 URL https://doi.org/10.24028/gzh.0203-3100.v34i3.2012.116637 [2] Borisov E K 2002 Security of the buildings located in the area of seismicaction of industrial explosions Thesis [3] Earthdoc 2020 Figure 1 https://www.earthdoc.org/content/figure/10.3997/2214- 4609.201902490.F1 [4] Feofanov A N 2009 Seismicheskaia aktivnost kak provotcirushchii faktor aktivizatcii protcessa sdvizheniia (Seismic activity as a provoking factor in the activation of the displacement process) Transactions of UkrNDMI NAN Ukraine 5 33–45 URL http://dspace.nbuv.gov.ua/handle/123456789/15921 [5] Feskova L 2015 Analysis of the technogenic seismicity problems Suchasni resursoenerhozberihaiuchi tekhnolohii hirnychoho vyrobnytstva 1 114–22 URL http://www.kdu.edu.ua/GV_jurnal/GV_1_2015(15)/114.pdf [6] Grachev A F, Magnitskiy V A, Mukhamediyev Sh A and Yunga S L 1996 Tensor characteristics of neotectonic flexural deformations and of curvature of the lithospheric basement surface on the East European platform Transactions (Doklady) of the Russian Academy of Sciences. Earth science sections. 343 46–53 [7] Kendzera O V 2015 Seismic hazard and seismic protection in Ukraine Ukrainian Geographical Journal 3 09–15 URL https://doi.org/10.15407/ugz2015.03.009 [8] Kutas V V, Omelchenko V D, Drogiczkaya G M and Kalitova I A 2009 Krivorozhskoe zemletryasenie 25 dekabrya 2007g (Krivoy Rog earthquake on December 25, 2007) Geofizicheskiy Zhurnal 31 42–52 [9] Nikonov A A 1984 Zemletriaseniia... Proshloe, sovremennost, prognoz (Earthquakes... Past, present, forecast) (Moscow: Znanie) p 73 [10] Paranko I S, Smyrnova A Ja and Ivanova O V 2005 Kryvyi Rih is a potential zone of technogenenatural and technogene extraordinary situations emergence Geology and Mineralogy Bulletin of Kryvyi Rih National University 13 5–9 URL https://drive.google.com/open?id=1- xRbXj49P_5qod8U1zqY5S0qGYADTiYn [11] Pigulevskiy P I, Svistun V K and Scherbina S V 2013 O tektonicheskom stroenii, geodinamicheskikh i sejsmologicheskikh osobennostyakh Krivbassa (On the tectonic structure, geodynamic and seismological features of Kryvbas) Ekologiya i prirodokoristuvannya 17 37–46 [12] Pustovitenko B G, Kulchitsky V E, Pustovitenko A A and Sklar A M 2010 Instrumental and macroseismic data on processes in the focal zone of the Krivoy Rog earthquake on December 25, 2007 Geofizicheskiy Zhurnal 32 75–97 URL https://doi.org/10.24028/gzh.0203- 3100.v32i2.2010.117558 [13] Pustovitenko B G, Pustovitenko A A and Kapitanova S A 2009 Proczesy v ochagovoj zone Krivorozhskogo zemletryaseniya 25 dekabrya 2007 g. (Processes in the focal zone of the Krivoy Rog earthquake on December 25, 2007) Sejsmologicheskij byulleten Ukrainy pp 17– 31 [14] Pіgulevskyi P H, Kendzera O V, Shcherbina S V, Verbytskyi S I, Shumlyanska L O, Kalinichenko O O, Gurova I Yu, Il’yenko V A, Amashukeli T A and Chalyi O O 2017 Nature of Krivyi Rih earthquake of July 29, 2017 Geology and Mineralogy Bulletin of Kryvyi Rih National University 37 92–106 URL https://drive.google.com/open?id=1riEKiq9Dgf2hXwOjZCOQRpvUl5AEUii [15] Sharov A V 2007 Zemletryaseniya i mikroseysmichnost' v zadachakh sovremennoy geodinamiki Vostochno Yevropeyskoy platformy (Earthquakes and microseismicity in the problems of modern geodynamics of the East European platform) vol 2 Microseismicity ed Sharov A V, Malichenko A A and Shchukin Yu K (Petrazavodsk: Karelian Scientific Center of the Russian Academy of Sciences) p 96 [16] Shcherbina S V, Pigulevskij P I, Gurova I Yu and Kalinichenko O A 2013 Registration and Anlisis of Natural and Man-Made Seismic Events in Krivoy Rog Geoinformatika 48 74–84 URL http://www.geology.com.ua/wp-content/uploads/2015/08/08_Sherbina.pdf [17] Shmandiy V M, Bredun V I and Kharlamova O V 2008 Rehionalni aspekty formuvannia seismichnoi skladovoi ekolohichnoi bezpeky (Regional aspects of the formation of the seismic component of environmental safety) Ekolohichna bezpeka 2 31–34 URL http://www.kdu.edu.ua/EKB_jurnal/2008_2(2)/31.pdf [18] Sklyar A M, Knyazeva V S and Ostanin A M 2007 Makrosejsmicheskij effekt Krivorozhskogo zemletryaseniya 25 dekabrya 2007 g. (Macroseismic effect of the Krivoy Rog earthquake on December 25, 2007) Sejsmologicheskij byulleten Ukrainy pp 48–53 [19] Tiapkin O K, Kendzera O V and Pihulevskyi P H 2017 Research of the Increased Induced Seismicity in Complex Geoecological Monitoring of Shallow Subsurface of Ukrainian Mini 23rd European Meeting of Environmental and Engineering Geophysics. Near Surface Geoscience’17 (Malmö, Sweden) vol 2017 pp 1–5 URL https://doi.org/10.3997/2214- 4609.201702055
dc.description.abstract	Information is provided on the number of earthquakes in Kryvyi Rih and their parameters for the period 2007–2018. The types of seismic phenomena, the criteria for their identification are considered. The most probable natural and technogenic factors of the epicenters of local earthquakes are established by analyzing their location and sequence in time from the point of view of the tectonic features of the territory and the nature of the technogenic interference in its structure. The necessity of creating a local seismological network in Kryvyi Rih is substantiated. With a view to predict hazardous seismic phenomena, there is a need to continue hydrogeodynamic monitoring of ground water, to introduce seismic gravity monitoring and to conduct microseismic monitoring at mining enterprises. The results of systematic monitoring shall serve as the basis for seismic microzoning of the city. It is emphasized that popularization and dissemination of knowledge about the seismicity of mining regions among the population shall play an important role in the implementation of this task. The research materials can be used in the master's degree programme within the framework of higher education system and in advanced training of specialists in the mining industry.	uk
dc.language.iso	en	uk
dc.publisher	IOP Publishing	uk
dc.subject	сейсмічність Кривого Рогу
dc.subject	сейсмічні явища
dc.subject	землетруси
dc.title	Analysis of natural and technogenic factors on the seismicity of Kryvyi Rih	uk
dc.type	Article	uk