{"id":234,"date":"2015-08-06T15:28:22","date_gmt":"2015-08-06T14:28:22","guid":{"rendered":"http:\/\/marine.geophysicsgpr.com\/?page_id=234"},"modified":"2017-02-27T16:55:12","modified_gmt":"2017-02-27T15:55:12","slug":"geologic-mapping","status":"publish","type":"page","link":"https:\/\/marine.geophysicsgpr.com\/en\/marine-geophysics-applications\/geological-and-geotechnical\/geologic-mapping","title":{"rendered":"Geologic Mapping"},"content":{"rendered":"
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As on land, there are a range of methodologies for geologic mapping of sub-surface bedrock and sediment layers.<\/p>\n

Different methods used for geologic mapping<\/h2>\n

Marine seismic refraction is the preferred methodology for engineering\/geotechnical studies where mapping the depth to competent bedrock is critical.<\/p>\n

Seismic reflection and sub-bottom profiling can produce detailed images of the subsurface layers.<\/p>\n

Side-scan sonar and bathymetry surveys are key components for mapping variations in bottom conditions.<\/p>\n

For more information, please contact our Marine Survey Team<\/a><\/span>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div>

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\n\t\t\"Geologic\n\t<\/div>\n\n<\/div><\/div><\/div><\/div>
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\n\t\t\"Geologic\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"

As on land, there are a range of methodologies for geologic mapping of sub-surface bedrock and sediment layers.Different methods used for geologic mappingMarine seismic refraction is the preferred methodology for engineering\/geotechnical studies where mapping the depth to competent bedrock is critical.Seismic reflection and sub-bottom profiling can produce detailed images of the subsurface layers.Side-scan sonar and… Read more »<\/a><\/p>\n","protected":false},"author":1,"featured_media":78,"parent":176,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-234","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/234","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/comments?post=234"}],"version-history":[{"count":12,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/234\/revisions"}],"predecessor-version":[{"id":1600,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/234\/revisions\/1600"}],"up":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/176"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media\/78"}],"wp:attachment":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media?parent=234"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}