{"id":738,"date":"2015-07-21T15:27:05","date_gmt":"2015-07-21T15:27:05","guid":{"rendered":"http:\/\/ground.geophysicsgpr.com\/?page_id=738"},"modified":"2018-05-19T22:19:27","modified_gmt":"2018-05-19T22:19:27","slug":"seismic-ground-geophysics-methods","status":"publish","type":"page","link":"https:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic-ground-geophysics-methods","title":{"rendered":"Seismic"},"content":{"rendered":"<div id=\"pl-738\"  class=\"panel-layout\" ><div id=\"pg-738-0\"  class=\"panel-grid panel-has-style\" ><div class=\"texte-home-right article panel-row-style panel-row-style-for-738-0\" ><div id=\"pgc-738-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-738-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p>Seismic ground geophysical methods are techniques based on the study of the propagation of seismic waves. The techniques outlined below involve\u00a0variations in data acquisition and processing, the choice of which will depend on the project goal. \u00a0Each technique can yield new insights into the subsurface.<\/p>\n<p>Follow the links below or contact our\u00a0<a href=\"mailto:info@geophysicsgpr.com\">Ground Survey Team<\/a>\u00a0to learn more.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-738-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-738-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-738-1-0-0\" class=\"so-panel widget widget_black-studio-tinymce widget_black_studio_tinymce panel-first-child panel-last-child\" data-index=\"1\" ><div class=\"textwidget\"><p><div id=\"wondergridgallerylightbox_options\" data-skinsfoldername=\"skins\/default\/\"  data-jsfolder=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/plugins\/wonderplugin-gridgallery\/engine\/\" style=\"display:none;\"><\/div>\r\n<style type=\"text\/css\">.wpp-btn-blue-medium {     background: #fa4c06; }  .wpp-btn-blue-medium:hover {     color: #fff;     background: #fa4c06; }<\/style><style type=\"text\/css\">@import url(https:\/\/fonts.googleapis.com\/css?family=Open+Sans);  #wonderplugingridgallery-4 .wonderplugin-gridgallery-item-text {     text-align: center;     box-sizing: border-box;     -webkit-box-sizing: border-box;     -moz-box-sizing: border-box; }  #wonderplugingridgallery-4 .wonderplugin-gridgallery-item-title {     font-family: 'Open Sans', sans-serif;     font-size: 18px;     position: absolute;     left: 5px;     top: 5px;     width: 97.5%;     height: auto;     background-color: #fa4c06;     color: #fff;     padding: 12px 5px; }  #wonderplugingridgallery-4 .wonderplugin-gridgallery-item-description {     font-size: 12px; }  #wonderplugingridgallery-4 .wonderplugin-gridgallery-item-button {     position: absolute;     right: 20px;     bottom: 20px; }  #wonderplugingridgallery-4 .wonderplugin-gridgallery-item-container img:hover { }<\/style><div class=\"wonderplugingridgallery\" id=\"wonderplugingridgallery-4\" data-gridgalleryid=\"4\" data-width=\"440\" data-height=\"350\" data-skin=\"threecolumns\" data-random=\"false\" data-shownavigation=\"true\" data-hoverzoomin=\"false\" data-hoverzoominimageonly=\"true\" data-hoverzoominimagecenter=\"false\" data-hoverfade=\"true\" data-responsive=\"true\" data-mediumscreen=\"true\" data-smallscreen=\"true\" data-showtitle=\"true\" data-showtexttitle=\"true\" data-showtextdescription=\"false\" data-showtextbutton=\"true\" data-lightboxnogroup=\"false\" data-lightboxshowtitle=\"true\" data-lightboxshowdescription=\"false\" data-lightboxresponsive=\"true\" data-circularimage=\"false\" data-firstimage=\"false\" data-textinsidespace=\"false\" data-thumbwidth=\"90\" data-thumbheight=\"60\" data-thumbtopmargin=\"12\" data-thumbbottommargin=\"4\" data-barheight=\"64\" data-titlebottomcss=\"{color:#333; font-size:14px; font-family:Armata,sans-serif,Arial; overflow:hidden; text-align:left;}\" data-descriptionbottomcss=\"{color:#333; font-size:12px; font-family:Arial,Helvetica,sans-serif; overflow:hidden; text-align:left; margin:4px 0px 0px; padding: 0px;}\" data-googleanalyticsaccount=\"\" data-gap=\"4\" data-margin=\"10\" data-borderradius=\"0\" data-hoverzoominvalue=\"24\" data-hoverzoominduration=\"180\" data-hoverzoominimagescale=\"1.1\" data-hoverzoominimageduration=\"360\" data-hoverfadeopacity=\"0.8\" data-hoverfadeduration=\"300\" data-videoplaybutton=\"playvideo-64-64-0.png\" data-column=\"3\" data-mediumcolumn=\"2\" data-mediumscreensize=\"800\" data-smallcolumn=\"1\" data-smallscreensize=\"600\" data-titlemode=\"always\" data-titleeffect=\"fade\" data-titleeffectduration=\"300\" data-titleheight=\"0\" data-jsfolder=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/plugins\/wonderplugin-gridgallery\/engine\/\" data-skinsfoldername=\"skins\/default\/\" style=\"display:none;position:relative;margin:0 auto;width:100%;max-width:1328px;\" ><div class=\"wonderplugin-gridgallery-list\" style=\"display:block;position:relative;max-width:100%;margin:0 auto;\"><div class=\"wonderplugin-gridgallery-item\" data-row=\"1\" data-col=\"1\"><div class=\"wonderplugin-gridgallery-item-container\"><a href=\"http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/refraction\/\" title=\"Refraction\" data-description=\"Refraction calculates seismic velocities and depths of the ground various layers.\" data-button=\"<a href=&quot;http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/refraction\/&quot;><button class=&quot;wpp-btn-blue-medium&quot;>Learn more<\/button><\/a>\"><img decoding=\"async\" class=\"wonderplugin-gridgallery-item-img\" src=\"http:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Techniques_Seismic_Refraction_1.jpg\" \/><\/a><\/div><\/div><div class=\"wonderplugin-gridgallery-item\" data-row=\"1\" data-col=\"1\"><div class=\"wonderplugin-gridgallery-item-container\"><a href=\"http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/reflection\/\" title=\"Reflection\" data-description=\"Reflection aims to capture and record the waves reflected by the various interfaces between horizons located in the studied area.\" data-button=\"<a href=&quot;http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/reflection\/&quot;><button class=&quot;wpp-btn-blue-medium&quot;>Learn more<\/button><\/a>\"><img decoding=\"async\" class=\"wonderplugin-gridgallery-item-img\" src=\"http:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/reflection-970x400.jpg\" \/><\/a><\/div><\/div><div class=\"wonderplugin-gridgallery-item\" data-row=\"1\" data-col=\"1\"><div class=\"wonderplugin-gridgallery-item-container\"><a href=\"http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/masw\/\" title=\"MASW\" data-description=\"Amos method (MASW) is commonly used to indirectly measure the profile of the shear wave velocities of the site materials.\" data-button=\"<a href=&quot;http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/masw\/&quot;><button class=&quot;wpp-btn-blue-medium&quot;>Learn more<\/button><\/a>\"><img decoding=\"async\" class=\"wonderplugin-gridgallery-item-img\" src=\"http:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/tech_masw-1024x768.jpg\" \/><\/a><\/div><\/div><div class=\"wonderplugin-gridgallery-item\" data-row=\"1\" data-col=\"1\"><div class=\"wonderplugin-gridgallery-item-container\"><a href=\"http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/resonance\/\" title=\"Hydro-Tisar\" data-description=\"Magnetic resonance survey is used to characterize aquifers and identify free hydrogen in the ground.\" data-button=\"<a href=&quot;http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/resonance\/&quot;><button class=&quot;wpp-btn-blue-medium&quot;>Learn more<\/button><\/a>\"><img decoding=\"async\" class=\"wonderplugin-gridgallery-item-img\" src=\"http:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/resonance-geophysique-terrestre-768x1024.jpg\" \/><\/a><\/div><\/div><div class=\"wonderplugin-gridgallery-item\" data-row=\"1\" data-col=\"1\"><div class=\"wonderplugin-gridgallery-item-container\"><a href=\"http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/acoustic-ndt\/\" title=\"Acoustic NDT\" data-description=\"Acoustic NDT is a technique measuring velocity propagation of high frequency seismic waves in concrete structures to assess their quality.\" data-button=\"<a href=&quot;http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/acoustic-ndt\/&quot;><button class=&quot;wpp-btn-blue-medium&quot;>Learn more<\/button><\/a>\"><img decoding=\"async\" class=\"wonderplugin-gridgallery-item-img\" src=\"http:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/08\/BFC_Valcartier_L11-018.jpg\" \/><\/a><\/div><\/div><div class=\"wonderplugin-gridgallery-item\" data-row=\"1\" data-col=\"1\"><div class=\"wonderplugin-gridgallery-item-container\"><a href=\"http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/borehole\/\" title=\"Borehole\" data-description=\"Used for the determination of rock or concrete quality and to detect faults and shear zones in bedrock.\" data-button=\"<a href=&quot;http:\/\/ground.geophysicsgpr.com\/en\/techniques\/seismic\/borehole\/&quot;><button class=&quot;wpp-btn-blue-medium&quot;>Learn more<\/button><\/a>\"><img decoding=\"async\" class=\"wonderplugin-gridgallery-item-img\" src=\"http:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/08\/DSCF1770.jpg\" \/><\/a><\/div><\/div><div style=\"clear:both;\"><\/div><\/div><div class=\"wonderplugin-gridgallery-engine\"><a href=\"http:\/\/www.wonderplugin.com\/wordpress-gridgallery\/\" title=\"WordPress Grid Gallery Plugin\">WordPress Grid Gallery Plugin<\/a><\/div><\/div><\/p>\n<\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Seismic ground geophysical methods are techniques based on the study of the propagation of seismic waves. The techniques outlined below involve\u00a0variations in data acquisition and processing, the choice of which will depend on the project goal. \u00a0Each technique can yield new insights into the subsurface.Follow the links below or contact our\u00a0Ground Survey Team\u00a0to learn more.<\/p>\n","protected":false},"author":1,"featured_media":3084,"parent":703,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-738","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/738","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/comments?post=738"}],"version-history":[{"count":2,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/738\/revisions"}],"predecessor-version":[{"id":3035,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/738\/revisions\/3035"}],"up":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/703"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media\/3084"}],"wp:attachment":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media?parent=738"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}