{"version":"1.0","provider_name":"smartTomo - imaging the subsurface of the Earth","provider_url":"https:\/\/www.smarttomo.com\/wp","author_name":"admin","author_url":"https:\/\/www.smarttomo.com\/wp\/author\/admin\/","title":"Tips on using dromochrones applied to seismic tomography - smartTomo - imaging the subsurface of the Earth","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"h84cu1rloZ\"><a href=\"https:\/\/www.smarttomo.com\/wp\/documents\/dromochrones_applied_to_seiemic_tomography\/\">Tips on using dromochrones applied to seismic tomography<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.smarttomo.com\/wp\/documents\/dromochrones_applied_to_seiemic_tomography\/embed\/#?secret=h84cu1rloZ\" width=\"600\" height=\"338\" title=\"&#8220;Tips on using dromochrones applied to seismic tomography&#8221; &#8212; smartTomo - imaging the subsurface of the Earth\" data-secret=\"h84cu1rloZ\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script>\n\/*! This file is auto-generated *\/\n!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);\n\/\/# sourceURL=https:\/\/www.smarttomo.com\/wp\/wp-includes\/js\/wp-embed.min.js\n<\/script>\n","description":"The dromochrone or travel-time curves are plots in which the arrival times of seismic waves are represented as a function of distance from the source. They find their use in localizing the position of earthquakes, in reflection and refraction seismic surveys. In this post we will address their use in refraction seismic and how they &hellip; Continue reading \"\"","thumbnail_url":"https:\/\/www.smarttomo.com\/wp\/wp-content\/uploads\/2021\/07\/rifrazione_FronteOnde-1024x358.png"}