1.0Сайт журналу «Геоінформатика»http://www.geology.com.ua/enАдміністраторhttp://www.geology.com.ua/en/blog/author/andriy/rich600338<blockquote class="wp-embedded-content" data-secret="6kLTWF5Cgj"><a href="http://www.geology.com.ua/en/2681-2/"></a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="http://www.geology.com.ua/en/2681-2/embed/#?secret=6kLTWF5Cgj" width="600" height="338" title="“” — Сайт журналу «Геоінформатика»" data-secret="6kLTWF5Cgj" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"></iframe><script type="text/javascript"> /* <![CDATA[ */ /*! This file is auto-generated */ !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); //# sourceURL=http://www.geology.com.ua/wp-includes/js/wp-embed.min.js /* ]]> */ </script> Geoinformatika 2012; 1(41) : 39-45 SPECTRAL EXPLORATION SEISMIC IN TECTONIC FAULTS MAPPING AND PREDICTION OF POSSIBLE DESTRUCTIONS IN THE AREA OF UNDERGROUND TUNNEL BETWEEN THE STATIONS “VASYLKIVSKA” – “EXHIBITION CENTRE”, KIEV A.G. Glikman, A.V. Danilov Method of spectral and seismic profiling (SSP) allows to solve the problems of searching of tectonic faults zones, geopathogenic zones, water deposits, various underground objects, to predict the destruction of engineering buildings, residential buildings, roadways, pipelines breaking. This method is an alternative to the traditional ones. Tectonic faults were identified and investigated; possible destructions in the area of underground tunnel between the stations “Vasylkivska”  – “Exhibition Centre” were predicted according to the profile data obtained by the SSP. Keywords: spectral exploration seismic, spectral and seismic profiling, tectonic faults zones, geopathogenic zones, fracture prediction.  http://www.geology.com.ua/wp-content/uploads/2013/09/pdf.jpg