{"id":1421,"date":"2016-11-16T09:52:26","date_gmt":"2016-11-16T09:52:26","guid":{"rendered":"http:\/\/ukogl.org.uk\/?p=1421"},"modified":"2017-01-30T13:22:08","modified_gmt":"2017-01-30T13:22:08","slug":"ukogl-archive-conoco-data","status":"publish","type":"post","link":"https:\/\/ukogl.org.uk\/blog\/ukogl-archive-conoco-data\/","title":{"rendered":"UKOGL Archive &#8211; Conoco Data"},"content":{"rendered":"<p>Two new Conoco surveys have been archived to UKOGL. The 1964 and 1965 vintage data sets consist of post stack SEG-Y and a scanned hard copy image for each line. The SEG-Y was reconstructed by scanning and vectorizing the sections.<\/p>\n<p>The1965 Gloucester survey is comprised of 7 lines NW of the Severn Estuary located over an area without any previous available seismic data.<\/p>\n<p><a href=\"https:\/\/ukogl.org.uk\/wp-content\/uploads\/2016\/11\/C65.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-1423\" src=\"https:\/\/ukogl.org.uk\/wp-content\/uploads\/2016\/11\/C65.jpg\" alt=\"C65 Seismic Lines\" width=\"1417\" height=\"853\" \/><\/a><\/p>\n<p>The 1964 Wigton survey is located in Cumbria complimenting the seismic coverage that is already available over this area.<\/p>\n<p><a href=\"https:\/\/ukogl.org.uk\/wp-content\/uploads\/2016\/11\/C64-W.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-1422\" src=\"https:\/\/ukogl.org.uk\/wp-content\/uploads\/2016\/11\/C64-W.jpg\" alt=\"c64-w\" width=\"1918\" height=\"899\" \/><\/a><\/p>\n<p>Both surveys can be licensed through UKOGL with high resolution JPEG images available for each line to provide an indication of data quality.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Two new Conoco surveys have been archived to UKOGL. The 1964 and 1965 vintage data sets consist of post stack SEG-Y and a scanned hard copy image for each line. The SEG-Y was reconstructed by scanning and vectorizing the sections. The1965 Gloucester survey is comprised of 7 lines NW of the Severn Estuary located over [&hellip;]<\/p>\n","protected":false},"author":3,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2],"tags":[],"class_list":["post-1421","post","type-post","status-publish","format-standard","hentry","category-seismic"],"_links":{"self":[{"href":"https:\/\/ukogl.org.uk\/blog\/wp-json\/wp\/v2\/posts\/1421","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ukogl.org.uk\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/ukogl.org.uk\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/ukogl.org.uk\/blog\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/ukogl.org.uk\/blog\/wp-json\/wp\/v2\/comments?post=1421"}],"version-history":[{"count":3,"href":"https:\/\/ukogl.org.uk\/blog\/wp-json\/wp\/v2\/posts\/1421\/revisions"}],"predecessor-version":[{"id":1489,"href":"https:\/\/ukogl.org.uk\/blog\/wp-json\/wp\/v2\/posts\/1421\/revisions\/1489"}],"wp:attachment":[{"href":"https:\/\/ukogl.org.uk\/blog\/wp-json\/wp\/v2\/media?parent=1421"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/ukogl.org.uk\/blog\/wp-json\/wp\/v2\/categories?post=1421"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/ukogl.org.uk\/blog\/wp-json\/wp\/v2\/tags?post=1421"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}