{"id":237,"date":"2021-06-21T22:19:48","date_gmt":"2021-06-21T10:19:48","guid":{"rendered":"https:\/\/blogs.otago.ac.nz\/keithgordon\/?p=237"},"modified":"2021-07-04T15:17:57","modified_gmt":"2021-07-04T03:17:57","slug":"new-publication-out-in-tectonophysics","status":"publish","type":"post","link":"https:\/\/blogs.otago.ac.nz\/keithgordon\/new-publication-out-in-tectonophysics\/","title":{"rendered":"New publication out in Tectonophysics"},"content":{"rendered":"<p><span class=\"d2edcug0 hpfvmrgz qv66sw1b c1et5uql lr9zc1uh a8c37x1j keod5gw0 nxhoafnm aigsh9s9 d3f4x2em fe6kdd0r mau55g9w c8b282yb iv3no6db jq4qci2q a3bd9o3v knj5qynh oo9gr5id hzawbc8m\" dir=\"auto\">Congratulations to <strong>Jeremy<\/strong> and <strong>Keith<\/strong> on their recent <a href=\"https:\/\/doi.org\/10.1016\/j.tecto.2021.228856\">publication<\/a> with VUW geologists. Using Raman microscopy it was possible to determine the pressures and temperatures to which the carbonaceous materials had been subjected. Along with other data the geology team were able to determine the age of the slip initiation (4 million years) in the Mai\u2019iu Fault in the Woodlark Rift of southeastern Papua New Guinea.<\/span><\/p>\n<p><a href=\"https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2021\/06\/2.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-244\" src=\"https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2021\/06\/2.jpg\" alt=\"\" width=\"581\" height=\"426\" srcset=\"https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2021\/06\/2.jpg 581w, https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2021\/06\/2-300x220.jpg 300w, https:\/\/blogs.otago.ac.nz\/keithgordon\/files\/2021\/06\/2-409x300.jpg 409w\" sizes=\"auto, (max-width: 581px) 100vw, 581px\" \/><\/a><\/p>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Congratulations to Jeremy and Keith on their recent publication with VUW geologists. Using Raman microscopy it was possible to determine the pressures and temperatures to which the carbonaceous materials had been subjected. Along with other data the geology team were able to determine the age of the slip initiation (4 million years) in the Mai\u2019iu [&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-237","post","type-post","status-publish","format-standard","hentry"],"_links":{"self":[{"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/posts\/237","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=237"}],"version-history":[{"count":0,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/posts\/237\/revisions"}],"wp:attachment":[{"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/media?parent=237"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/categories?post=237"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.otago.ac.nz\/keithgordon\/wp-json\/wp\/v2\/tags?post=237"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}