{"id":19768,"date":"2019-06-04T18:57:30","date_gmt":"2019-06-04T16:57:30","guid":{"rendered":"http:\/\/karmaka.de\/?p=19768"},"modified":"2019-06-04T18:57:31","modified_gmt":"2019-06-04T16:57:31","slug":"formation-parameters-of-high-pressure-minerals-in-the-dhofar-717-and-864-chondrite-meteorites","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=19768","title":{"rendered":"Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites"},"content":{"rendered":"\n<p>K. D. Litasov, D. D. Badyukov, N. P. Pokhilenko<\/p>\n\n\n\n<p>Doklady Earth Sciences<br>\nMarch 2019, Volume 485, Issue 1, pp 327-330<br>\nFirst Online: 28 May 2019<\/p>\n\n\n\n<p><a href=\"https:\/\/link.springer.com\/article\/10.1134%2FS1028334X19030322\" target=\"_blank\" rel=\"noreferrer noopener\"><strong>LINK<\/strong><\/a><\/p>\n\n\n\n<p class=\"justify-text\">&#8220;This paper presents the results of a Raman spectroscopic study of shock melt veins in L6 chondritic meteorites Dhofar 717 and 864, and conclusions about the P\u2013T parameters recorded in these meteorites after the impact event. The primary minerals of the host chondrite include olivine, orthopyroxene, clinopyroxene, plagioclase, chromite, phosphates, troilite, and kamasite. Shock melt veins up to 1 cm thick contain fragments of the high-pressure minerals ringwoodite, wadsleyite, majorite, akimotoite, jadeite, lingunite, and tuite and quenched melt consisting of majorite, ringwoodite, troilite, and kamasite. The mineral associations of the Dhofar 717 and 864 chondrites indicate high peak PT parameters of the impact in the region of stability of majorite (&gt;20 GPa and &gt;2500 K) and bridgmanite (&gt;25 GPa and &gt;2500 K). The presence of lingunite also directly indicates a peak pressure in the area of stability of the bridgmanite.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>K. D. Litasov, D. D. Badyukov, N. P. Pokhilenko Doklady Earth Sciences March 2019, Volume 485, Issue 1, pp 327-330 First Online: 28 May 2019 LINK &#8220;This paper presents the results of a Raman spectroscopic&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[23,7,63],"tags":[5012,5013,2805,1815,3968,1807,264],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/19768"}],"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=19768"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/19768\/revisions"}],"predecessor-version":[{"id":19769,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/19768\/revisions\/19769"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=19768"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=19768"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=19768"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}