{"id":348,"date":"2022-05-14T15:04:16","date_gmt":"2022-05-14T03:04:16","guid":{"rendered":"https:\/\/blogs.otago.ac.nz\/keithgordon\/?p=348"},"modified":"2022-05-14T15:04:44","modified_gmt":"2022-05-14T03:04:44","slug":"348-2","status":"publish","type":"post","link":"https:\/\/blogs.otago.ac.nz\/keithgordon\/348-2\/","title":{"rendered":"Recent publication in European Journal of Mineralogy"},"content":{"rendered":"<p>Jeremy and Keith recently published work with the Otago Department of Geology (Matthew Tarling and Steven Smith) entitled \u201cCrystallographic orientation mapping of lizardite serpentinite by Raman spectroscopy\u201d in the <em>European Journal of Mineralogy<\/em> (2022) 34, 285 \u2013 300 \u00a0<a href=\"https:\/\/doi.org\/10.5194\/ejm-34-285-2022\">https:\/\/doi.org\/10.5194\/ejm-34-285-2022<\/a><\/p>\n<p><a href=\"https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2022\/05\/Raman-spectra.png\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-large wp-image-349\" src=\"https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2022\/05\/Raman-spectra-1024x404.png\" alt=\"\" width=\"1024\" height=\"404\" srcset=\"https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2022\/05\/Raman-spectra-1024x404.png 1024w, https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2022\/05\/Raman-spectra-300x118.png 300w, https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2022\/05\/Raman-spectra-768x303.png 768w, https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2022\/05\/Raman-spectra-500x197.png 500w, https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2022\/05\/Raman-spectra.png 1042w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><\/p>\n<p>This shows the importance of crystal orientation for observed Raman spectra and can be used to explain some phenomena within the literature.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Jeremy and Keith recently published work with the Otago Department of Geology (Matthew Tarling and Steven Smith) entitled \u201cCrystallographic orientation mapping of lizardite serpentinite by Raman spectroscopy\u201d in the European Journal of Mineralogy (2022) 34, 285 \u2013 300 \u00a0https:\/\/doi.org\/10.5194\/ejm-34-285-2022 This shows the importance of crystal orientation for observed Raman spectra and can be used to [&hellip;]<\/p>\n","protected":false},"author":33170,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[],"tags":[],"class_list":["post-348","post","type-post","status-publish","format-standard","hentry"],"_links":{"self":[{"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/posts\/348","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\/33170"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/comments?post=348"}],"version-history":[{"count":0,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/posts\/348\/revisions"}],"wp:attachment":[{"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/media?parent=348"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/categories?post=348"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/tags?post=348"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}