{"id":4497,"date":"2016-03-02T13:46:50","date_gmt":"2016-03-02T13:46:50","guid":{"rendered":"http:\/\/blog.soton.ac.uk\/ggblog\/?p=4497"},"modified":"2016-03-02T13:51:02","modified_gmt":"2016-03-02T13:51:02","slug":"pilab-project-sails-through-with-cruise-blog-now-live","status":"publish","type":"post","link":"https:\/\/blog.soton.ac.uk\/ggblog\/2016\/03\/pilab-project-sails-through-with-cruise-blog-now-live\/","title":{"rendered":"PILAB project sails through (cruise blog now live)"},"content":{"rendered":"

The P<\/strong>assive I<\/strong>maging of the L<\/strong>ithosphere and A<\/strong>sthenosphere B<\/strong>oundary project\u00a0aims at studying the interaction of the base of the rigid tectonic part (the lithosphere) with the softer layer underneath it \u2013 the asthenosphere. Understanding interaction between the two layers is essential in order to better understand what makes plates \u2018plate-like\u2019, and thus understanding the origin of continents, ocean basins and mountain ranges. To achieve this, Ocean Bottom Seismometers (OBS) and Ocean Bottom Electro-Magnetic (OBEM) instruments will be deployed across the Mid-Atlantic Ridge along the equator. The instruments will be left at sea for a couple of months to record seismic vibrations and measure the Earth\u2019s electro-magnetic field. The data will eventually be used to map the Earth\u2019s interior structure beneath.<\/p>\n

This project is a collaboration between various institutions that are providing the instruments and technical expertise\u00a0including\u00a0Institut de Physique du Globe de Paris (IPGP), Lamont-Doherty Earth Observatory (LDEO) from the University of Columbia, Scripps Institute of Oceanography (SIO) from the University of San Diego, University of Southampton (UoS), University of Bristol, and GEOMAR from Helmholtz Centre for Ocean Research, Kiel. \u00a0The funding is provided by the Natural Environment Research Council (NERC), the European Research Council (ERC), and the National Science Foundation (NSF). The Principal Investigator of the mission is Catherine A. Rychert<\/a> from the University of Southampton.<\/p>\n

Please visit the dedicated cruise blog:\u00a0https:\/\/pilabsoton.wordpress.com<\/a>\/<\/p>\n

(or click the icon on the side menu)<\/p>\n

\"Scientific<\/a>
Scientific party briefing and safety orientation<\/figcaption><\/figure>\n
\"R\/V<\/a>
R\/V Marcus G. Langseth berthed at Porto Grande, Cape Verde<\/figcaption><\/figure>\n
\"Ships<\/a>
Ships deck loaded with the ocean bottom instruments<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"

The Passive Imaging of the Lithosphere and Asthenosphere Boundary project\u00a0aims at studying the interaction of the base of the rigid tectonic part (the lithosphere) with the softer layer underneath it \u2013 the asthenosphere. Understanding interaction between the two layers is essential in order to better understand what makes plates \u2018plate-like\u2019, and thus understanding the origin… Read More PILAB project sails through (cruise blog now live)<\/span><\/a><\/p>\n","protected":false},"author":64890,"featured_media":4498,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"link","meta":{"ngg_post_thumbnail":0,"footnotes":""},"categories":[493988,78047,4217,493990],"tags":[69622,786433,786432,493999],"class_list":["post-4497","post","type-post","status-publish","format-link","has-post-thumbnail","hentry","category-blog-roll","category-fieldwork","category-news","category-science-cruises","tag-geophysics","tag-ocean-bottom-seismometers","tag-passive-imaging-seismic-imaging","tag-seismology","post_format-post-format-link"],"_links":{"self":[{"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/posts\/4497","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/users\/64890"}],"replies":[{"embeddable":true,"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/comments?post=4497"}],"version-history":[{"count":3,"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/posts\/4497\/revisions"}],"predecessor-version":[{"id":4503,"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/posts\/4497\/revisions\/4503"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/media\/4498"}],"wp:attachment":[{"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/media?parent=4497"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/categories?post=4497"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blog.soton.ac.uk\/ggblog\/wp-json\/wp\/v2\/tags?post=4497"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}