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="L6GrRbgFg3"><a href="http://www.geology.com.ua/en/2597-2/"></a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="http://www.geology.com.ua/en/2597-2/embed/#?secret=L6GrRbgFg3" width="600" height="338" title="“” — Сайт журналу «Геоінформатика»" data-secret="L6GrRbgFg3" 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; 3(43) : 33-40 ENERGY APPROACH TO THE ANALYSIS OF THE WAVE FIELD AS A CONCEPT OF THE SEISMIC DATA INVERSION Yu.P. Starodub, A.V. Karpenko The article discusses a general concept of the modern methods of inversion and a concept of the seismic data inversion based on the concepts of energy excitation, propagation and recording of elastic waves, which allows to calculate average and interval velocity of longitudinal waves, as well as density, porosity, acoustic impedance, Poisson’s ratio of the observable environment. The proposed method makes it possible to reverse the dynamic transformation of seismic traces data into geological section. Keywords: energy method, wave field, geophysical parameters, geological environment, inversion, seismic exploration.http://www.geology.com.ua/wp-content/uploads/2013/09/pdf.jpg