{"id":9873,"date":"2016-09-12T21:22:13","date_gmt":"2016-09-12T19:22:13","guid":{"rendered":"http:\/\/karmaka.de\/?p=9873"},"modified":"2016-09-12T21:22:13","modified_gmt":"2016-09-12T19:22:13","slug":"core-merging-and-stratification-following-giant-impact","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=9873","title":{"rendered":"Core merging and stratification following giant impact"},"content":{"rendered":"<p>Maylis Landeau, Peter Olson, Renaud Deguen &#038; Benjamin H. Hirsh<\/p>\n<p>Nature Geoscience(2016)<br \/>\ndoi:10.1038\/ngeo2808<br \/>\nPublished online 12 September 2016 <\/p>\n<p><a href=\"http:\/\/www.nature.com\/ngeo\/journal\/vaop\/ncurrent\/full\/ngeo2808.html\" target=\"_blank\"><strong>LINK<\/strong><\/a><\/p>\n<p>&#8220;A stratified layer below the core\u2013mantle boundary has long been suspected on the basis of geomagnetic and seismic observations1, 2, 3. It has been suggested that the outermost core has a stratified layer about 100\u2009km thick3, 4, 5, 6 that could be due to the diffusion of light elements7, 8. Recent seismological evidence, however, supports a layer exceeding 300\u2009km in thickness of enigmatic origin9, 10, 11. Here we show from turbulent mixing experiments that merging between projectile and planetary core following a giant impact can lead to a stratified layer at the top of the core. Scaling relationships between post-impact core structure and projectile properties suggest that merging between Earth\u2019s protocore and a projectile core that is enriched in light elements and 20 times less massive can produce the thick stratification inferred from seismic data. Our experiments favour Moon-forming impact scenarios involving a projectile smaller than the proto-Earth12, 13 and suggest that entrainment of mantle silicates into the protocore led to metal\u2013silicate equilibration under extreme pressure\u2013temperature conditions. We conclude that the thick stratified layer detected at the top of Earth\u2019s core9, 10 can be explained as a vestige of the Moon-forming giant impact during the late stages of planetary accretion.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Maylis Landeau, Peter Olson, Renaud Deguen &#038; Benjamin H. Hirsh Nature Geoscience(2016) doi:10.1038\/ngeo2808 Published online 12 September 2016 LINK &#8220;A stratified layer below the core\u2013mantle boundary has long been suspected on the basis of geomagnetic&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[131,922,72,112,115,71],"tags":[3235,80,3234,113,1857,1665],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/9873"}],"collection":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=9873"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/9873\/revisions"}],"predecessor-version":[{"id":9874,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/9873\/revisions\/9874"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=9873"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=9873"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=9873"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}