<?xml version="1.0"?>
<oembed><version>1.0</version><provider_name>&#x421;&#x430;&#x439;&#x442; &#x436;&#x443;&#x440;&#x43D;&#x430;&#x43B;&#x443; &#xAB;&#x413;&#x435;&#x43E;&#x456;&#x43D;&#x444;&#x43E;&#x440;&#x43C;&#x430;&#x442;&#x438;&#x43A;&#x430;&#xBB;</provider_name><provider_url>http://www.geology.com.ua/en</provider_url><author_name>&#x410;&#x434;&#x43C;&#x456;&#x43D;&#x456;&#x441;&#x442;&#x440;&#x430;&#x442;&#x43E;&#x440;</author_name><author_url>http://www.geology.com.ua/en/blog/author/andriy/</author_url><title>2009; 1 : 69-81 - &#x421;&#x430;&#x439;&#x442; &#x436;&#x443;&#x440;&#x43D;&#x430;&#x43B;&#x443; &#xAB;&#x413;&#x435;&#x43E;&#x456;&#x43D;&#x444;&#x43E;&#x440;&#x43C;&#x430;&#x442;&#x438;&#x43A;&#x430;&#xBB;</title><type>rich</type><width>600</width><height>338</height><html>&lt;blockquote class="wp-embedded-content" data-secret="zTz5TEtMJ6"&gt;&lt;a href="http://www.geology.com.ua/en/2009-1-69-81/"&gt;2009; 1 : 69-81&lt;/a&gt;&lt;/blockquote&gt;&lt;iframe sandbox="allow-scripts" security="restricted" src="http://www.geology.com.ua/en/2009-1-69-81/embed/#?secret=zTz5TEtMJ6" width="600" height="338" title="&#x201C;2009; 1 : 69-81&#x201D; &#x2014; &#x421;&#x430;&#x439;&#x442; &#x436;&#x443;&#x440;&#x43D;&#x430;&#x43B;&#x443; &#xAB;&#x413;&#x435;&#x43E;&#x456;&#x43D;&#x444;&#x43E;&#x440;&#x43C;&#x430;&#x442;&#x438;&#x43A;&#x430;&#xBB;" data-secret="zTz5TEtMJ6" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"&gt;&lt;/iframe&gt;&lt;script type="text/javascript"&gt;
/* &lt;![CDATA[ */
/*! This file is auto-generated */
!function(d,l){"use strict";l.querySelector&amp;&amp;d.addEventListener&amp;&amp;"undefined"!=typeof URL&amp;&amp;(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&amp;&amp;!/[^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&lt;o.length;i++)o[i].style.display="none";for(i=0;i&lt;a.length;i++)s=a[i],e.source===s.contentWindow&amp;&amp;(s.removeAttribute("style"),"height"===t.message?(1e3&lt;(r=parseInt(t.value,10))?r=1e3:~~r&lt;200&amp;&amp;(r=200),s.height=r):"link"===t.message&amp;&amp;(r=new URL(s.getAttribute("src")),n=new URL(t.value),c.test(n.protocol))&amp;&amp;n.host===r.host&amp;&amp;l.activeElement===s&amp;&amp;(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&lt;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
/* ]]&gt; */
&lt;/script&gt;
</html><description>Geoinformatika 2009; 1 :&#xA0;69-81 LANDSCAPE GEOINDICATORS OF FRACTURES&#x2019; DESCRIPTIONS AS A FOUNDATION OF THEIR RESEARCH BY REMOTE SENSING METHODS. 1. MORPHOKINEMATIC FEATURES OF DISJUNCTIVE STRUCTURES Azimov O.T. The article presents basic features of kinematic descriptions of the Earth&#x2019;s crust disjunctive structures in the main constituent of the recent landscape for the day surface. There are also described peculiarities of reflecting the features in remote sensing data. The features are for conditions of platform areas.</description><thumbnail_url>http://www.geology.com.ua/wp-content/uploads/2013/09/pdf.jpg</thumbnail_url></oembed>
