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="P4Y58hKmuF"><a href="http://www.geology.com.ua/en/geoinformatika-2016-359-14-19/">Geoinformatika 2016; 3(59) : 14-19</a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="http://www.geology.com.ua/en/geoinformatika-2016-359-14-19/embed/#?secret=P4Y58hKmuF" width="600" height="338" title="“Geoinformatika 2016; 3(59) : 14-19” — Сайт журналу «Геоінформатика»" data-secret="P4Y58hKmuF" 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 2016; 3(59) : 14-19  (in Ukrainian) Paleo-Channels Prediction in Carboniferous Sediments of the South-East Part of the Dnieper-Donets Basin (Based on the Results of Siesmic-Facies Analysis) N.I. Nesina, G.G. Markova LLC “Vikoil LTD”, 7 Kudryavsky uzviz Str., of. 920, Kyiv 04053, Ukraine, e-mail: natalia_nesina@bigmir.net, galina.markova@ubseismic.com The purpose of the paper is to show the efficacy of seismic-facies analysis for more specific application of 3D seismic to predict lithological hydrocarbon traps. The analysis was carried out in the South-East part of the Dnieper-Donets Basin for the sediments of Carboneferous on the sides of an anticline fold formed during a salt dome structure growing. Design/methodology/approach. Predictions were carried out using Neural Network Technology (NNT) seismic traces classification to obtain seismic facies distribution. Findings. The prediction areas of paleo-channels location were identified in the intervals of the Middle and Upper Carboniferous sediments based on the results of seismic-facies analysis. The results of the seismic-facies maps analysis, vertical sections and horizon slices of the seismic cube with amplitude anomalies corresponding to paleo-channels, allowed us to suppose that these paleo-channels were formed under different conditions of sedimentation. These conditions were connected with global sea level variations and with local tectonic movements caused by salt-dome structure forming. Practical value/implications. Paleo-channels, as the lithological bodies, are quite promising for potential non-anticline hydrocarbon traps forming. The latter has been constantly confirmed by Ukrainian and foreign geologists. Keywords: seismic-facies analysis, paleo-channel, horizon slice, Dnieper-Donets Basin, Pennsylvanian. The full text of papers