{"version":"1.0","provider_name":"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","provider_url":"http:\/\/www.geology.com.ua\/en","author_name":"\u0410\u0434\u043c\u0456\u043d\u0456\u0441\u0442\u0440\u0430\u0442\u043e\u0440","author_url":"http:\/\/www.geology.com.ua\/en\/blog\/author\/andriy\/","title":"(\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430) Geoinformatika 2014; 2(50) : 70-76 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"6GbR364aQ0\"><a href=\"http:\/\/www.geology.com.ua\/en\/2199-2\/\">(\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430) Geoinformatika 2014; 2(50) : 70-76<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"http:\/\/www.geology.com.ua\/en\/2199-2\/embed\/#?secret=6GbR364aQ0\" width=\"600\" height=\"338\" title=\"&#8220;(\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430) Geoinformatika 2014; 2(50) : 70-76&#8221; &#8212; \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\" data-secret=\"6GbR364aQ0\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script type=\"text\/javascript\">\n\/* <![CDATA[ *\/\n\/*! This file is auto-generated *\/\n!function(d,l){\"use strict\";l.querySelector&&d.addEventListener&&\"undefined\"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!\/[^a-zA-Z0-9]\/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret=\"'+t.secret+'\"]'),o=l.querySelectorAll('blockquote[data-secret=\"'+t.secret+'\"]'),c=new RegExp(\"^https?:$\",\"i\"),i=0;i<o.length;i++)o[i].style.display=\"none\";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute(\"style\"),\"height\"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):\"link\"===t.message&&(r=new URL(s.getAttribute(\"src\")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener(\"message\",d.wp.receiveEmbedMessage,!1),l.addEventListener(\"DOMContentLoaded\",function(){for(var e,t,s=l.querySelectorAll(\"iframe.wp-embedded-content\"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute(\"data-secret\"))||(t=Math.random().toString(36).substring(2,12),e.src+=\"#?secret=\"+t,e.setAttribute(\"data-secret\",t)),e.contentWindow.postMessage({message:\"ready\",secret:t},\"*\")},!1)))}(window,document);\n\/\/# sourceURL=http:\/\/www.geology.com.ua\/wp-includes\/js\/wp-embed.min.js\n\/* ]]> *\/\n<\/script>\n","description":"Geoinformatika 2014; 2(50) :\u00a070-76 (in Ukrainian) TECTONIC POSITION AND FOCAL AND DYNAMIC PARAMETERS OF THE KOMARNE EARTHQUAKE IN LVIV REGION L.Ye. Nazarevych Institute of Geophysics of NAS of Ukraine, ave Palladin, 32, Kiev 03680, Ukraine, e-mail: nazarevych.l@gmail.com Lviv region territory belongs to a 6-point seismic zone. It is the contact area of West and East Europan platforms. The purpose of the article is to study local earthquakes as an indicator of geodynamic activity of this area. Over a historical period (from 1000 AD), a number of earthquakes with the I\u00a0=\u00a05\u00b86\u00a0 have occurred here; for three of them (Shklo, 1670; V. Mosty, 1875; Komarne, 2007) localization of the sources was defined. The study gives a brief geological and tectonic characteristic of their focal zones. The authors traced the connection between these earthquakes and vertical Holocene movements of Volyno-Podolia and Precarpathians territory. The10.11.2007 earthquake with a magnitude of \u041cD\u00a0=\u00a02,3 and epicenter in the village Komarne (Lviv region) was considered in detail, which indicates the recent activity of the territory. By a complex of geological and geophysical data, the authors analyzed the localization of this earthquake source in relation to tectonic structures of the subregion and to the features of its modern geodynamics. It was determined that the earthquake source is confined to the Gorodok fault. The features of the wave pattern of this earthquake were analyzed. By the azimuthal hodograph method, the authors determined the break propagation directions in this source, and found that the direction of the main break coincides in plan with the Gorodok fault. The study determines focal and dynamic parameters of this earthquake, which indicate the distribution of the break along the prearranged geological fault. Characteristics of the modern state of the seismotectonic activity of the Gorodok fault were given. Keywords: Lviv region, \u0435arthquake, tectonic, focal and dynamic parameters. The full text of papers\u00a0 References Bugaev E.G. O strukturirovannoj i rassejanoj sejsmichnosti, zhestkosti ochagov zemletrjasenij i nelinejnosti grafikov povtorjaemosti magnitud [On structured and diffuse seismicity, stiffness of earthquake foci, and nonlinearity of magnitude recurrence graphs]. Geodinamika i tektonofizika [Geodynamics and Tectonophysics], 2011, vol. 2, pp. 244-265. Herenchuk K.I. Pryroda L\u2019vivs\u2019koyi oblasti [Nature of Lviv region]. Lviv, Vyd-vo L\u2019viv. univ., 1972, 145 p. Gorbunova I.V. Opredelenie protjazhennosti ochaga i napravlenija razryva po volnovoj kartine na sejsmogramme [Determination of length of focus and the direction of break by the wave form on the seismogram]. 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Pustovitenko [Seismological bulletin of Ukraine, 2007. By ed. of B.G. Pustovitenko]. Sevastopol: NPC \u201cEKOSI-Gidrofizika\u201d [RPC \u201cEKOSI-Hydrophysics\u201d], 2008, 252 p. Tektonichna karta Zakhidnoho naftohazonosnoho rehionu Ukrayiny [Karty] [Tectonic map of Western oil and gas region of Ukraine]. Kyiv, Ukrayins\u2019kyy derzhavnyy heolohorozviduval\u2019nyy instytut [Ukrainian State Geological Prospecting Institute], 1994. Gordienko V.V., Gordienko I.V., Zavgorodnjaja O.V., Kovachikova S., Logvinov I.M., Tarasov V.M., Usenko O.V. Ukrainskie Karpaty (geofizika, glubinnye processy) [Ukrainian Carpathians (geophysics, deep processes)]. Kyiv, Logos, 2011, 129 p. Brune J.N. Tectonic stress and the spectra of seismic shear waves from earthquakes. Journal of Geophysical Research, 1970, vol. 75, no 26, pp. 4997\u20135009. \/\/"}