{"id":11712,"date":"2017-02-14T14:21:18","date_gmt":"2017-02-14T13:21:18","guid":{"rendered":"http:\/\/karmaka.de\/?p=11712"},"modified":"2017-02-14T14:21:18","modified_gmt":"2017-02-14T13:21:18","slug":"spherulite-like-jadeite-growth-in-shock-melt-veins-of-the-novosibirsk-h56-chondrite","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=11712","title":{"rendered":"\u201cSpherulite-like\u201d jadeite growth in shock-melt veins of the Novosibirsk H5\/6 chondrite"},"content":{"rendered":"<p>I.S. Bazhan, Shin Ozawa, M. Miyahara, E. Ohtani, K.D. Litasov<\/p>\n<p>Russian Geology and Geophysics<br \/>\nVolume 58, Issue 1, January 2017, Pages 12\u201319<br \/>\nReceived 3 December 2015, Accepted 26 April 2016, Available online 13 February 2017<\/p>\n<p><a href=\"http:\/\/www.sciencedirect.com\/science\/article\/pii\/S1068797116302565\" target=\"_blank\"><strong>LINK<\/strong><\/a><\/p>\n<p>&#8220;The Novosibirsk H5\/6 ordinary chondrite has signs of shock metamorphism, such as dark shock-melt veins (SMVs) crossing the chondrite host rock. The plagioclase composition grains (Ab78An14Or7) with jadeite were found in the host-rock fragments inside the SMVs. Jadeite has an unusual radial-concentric spherulite-like microtexture. The spherulite-like jadeite formed from the molten plagioclase grain under high-pressure and high-temperature conditions during an impact event. The crystallization was accompanied by sodium-potassium differentiation between coexisting jadeite and residual melt. The PT-conditions of jadeite formation were estimated to be 3-14 GPa and 1400-2150 \u00b0C. Jadeite crystallization, Na-K differentiation, and the pressure-temperature estimates of jadeite formation in the Novosibirsk chondrite are very close to those in the Chelyabinsk LL5 chondrite. The spherulite-like microtexture and jadeite-glass coexistence, most likely, point to a high cooling rate of the SMVs at the pressure release stage of the metamorphic process.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>I.S. Bazhan, Shin Ozawa, M. Miyahara, E. Ohtani, K.D. Litasov Russian Geology and Geophysics Volume 58, Issue 1, January 2017, Pages 12\u201319 Received 3 December 2015, Accepted 26 April 2016, Available online 13 February 2017&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[6,7,63],"tags":[1806,3199,3655,3596,1807,3656],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/11712"}],"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=11712"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/11712\/revisions"}],"predecessor-version":[{"id":11713,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/11712\/revisions\/11713"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=11712"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=11712"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=11712"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}