{"id":249,"date":"2021-07-19T15:02:19","date_gmt":"2021-07-19T03:02:19","guid":{"rendered":"https:\/\/blogs.otago.ac.nz\/keithgordon\/?p=249"},"modified":"2021-07-19T15:02:19","modified_gmt":"2021-07-19T03:02:19","slug":"new-publication-out-in-earth-and-planetary-science-letters","status":"publish","type":"post","link":"https:\/\/blogs.otago.ac.nz\/keithgordon\/new-publication-out-in-earth-and-planetary-science-letters\/","title":{"rendered":"New publication out in  Earth and Planetary Science Letters"},"content":{"rendered":"<p><a href=\"https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2021\/07\/keith-jeremy-768x395-1.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-250\" src=\"https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2021\/07\/keith-jeremy-768x395-1.jpg\" alt=\"\" width=\"768\" height=\"395\" srcset=\"https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2021\/07\/keith-jeremy-768x395-1.jpg 768w, https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2021\/07\/keith-jeremy-768x395-1-300x154.jpg 300w, https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2021\/07\/keith-jeremy-768x395-1-500x257.jpg 500w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><\/a><\/p>\n<p>Congratulations to <em><strong>Jeremy<\/strong><\/em> and <em><strong>Keith<\/strong><\/em> who published a paper, in collaboration with the Department of Geology, entitled \u201cA common type of mineralogical banding in serpentine crack-seal veins\u201d.<\/p>\n<p>In this paper published in Earth and Planetary Science Letters (<a href=\"https:\/\/doi.org\/10.1016\/j.epsl.2021.116930\" target=\"_blank\" rel=\"noopener noreferrer\">https:\/\/doi.org\/10.1016\/j.epsl.2021.116930<\/a>), Raman spectroscopy is able to detect the incredibly narrow bands of chrysotile within lizardite. Using a variety of samples from around the world it is shown that this Raman-based technology may be used for a host of samples. The Geology suggests that recurrent small earthquakes lead to the banding.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Congratulations to Jeremy and Keith who published a paper, in collaboration with the Department of Geology, entitled \u201cA common type of mineralogical banding in serpentine crack-seal veins\u201d. In this paper published in Earth and Planetary Science Letters (https:\/\/doi.org\/10.1016\/j.epsl.2021.116930), Raman spectroscopy is able to detect the incredibly narrow bands of chrysotile within lizardite. Using a variety [&hellip;]<\/p>\n","protected":false},"author":35380,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[],"tags":[],"class_list":["post-249","post","type-post","status-publish","format-standard","hentry"],"_links":{"self":[{"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/posts\/249","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/users\/35380"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/comments?post=249"}],"version-history":[{"count":0,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/posts\/249\/revisions"}],"wp:attachment":[{"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/media?parent=249"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/categories?post=249"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/tags?post=249"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}