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="bwqwo8bLmP"><a href="http://www.geology.com.ua/en/2643-2/"></a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="http://www.geology.com.ua/en/2643-2/embed/#?secret=bwqwo8bLmP" width="600" height="338" title="“” — Сайт журналу «Геоінформатика»" data-secret="bwqwo8bLmP" 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; 2(42) : 38-43 INCREASE OF VERTICAL RESOLUTION FOR LOW-FREQUENCY INDUCTION LOGGING ON THE BASE OF SOLVING THE FIRST KIND FREDHOLM EQUATION OF CONVOLUTION TYPE N.L. Mirontsov Described in the paper is an algorithm of solving the first kind Fredholm equation of convolution type, which  permits to increase vertical resolution for low-frequency induction logging up to the value comparable with a recording step. Some examples of effective inverse solution with using such algorithm for thin-layer cross-sections are given. Keywords: inverse problem, induction logging, Fredholm equation, kernel of convolution type.http://www.geology.com.ua/wp-content/uploads/2013/09/pdf.jpg