{"id":8822,"date":"2016-06-03T06:44:56","date_gmt":"2016-06-03T04:44:56","guid":{"rendered":"http:\/\/karmaka.de\/?p=8822"},"modified":"2016-06-03T06:44:56","modified_gmt":"2016-06-03T04:44:56","slug":"high-pressure-phases-in-shock-induced-melt-of-the-unique-highly-shocked-ll6-chondrite-northwest-africa-757","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=8822","title":{"rendered":"High-pressure phases in shock-induced melt of the unique highly shocked LL6 chondrite Northwest Africa 757."},"content":{"rendered":"<p>Hu, J. and Sharp, T. G.<\/p>\n<p>Meteoritics &#038; Planetary Science. doi: 10.1111\/maps.12672<\/p>\n<p><a href=\"http:\/\/onlinelibrary.wiley.com\/doi\/10.1111\/maps.12672\/abstract\" target=\"_blank\"><strong>LINK<\/strong><\/a><\/p>\n<p>&#8220;Northwest Africa 757 is unique in the LL chondrite group because of its abundant shock-induced melt and high-pressure minerals. Olivine fragments entrained in the melt transform partially and completely into ringwoodite. Plagioclase and Ca-phosphate transform to maskelynite, lingunite, and tuite. Two distinct shock-melt crystallization assemblages were studied by FIB-TEM analysis. The first melt assemblage, which includes majoritic garnet, ringwoodite plus magnetite-magnesiow\u00fcstite, crystallized at pressures of 20\u201325 GPa. The other melt assemblage, which consists of clinopyroxene and wadsleyite, solidified at ~15 GPa, suggesting a second veining event under lower pressure conditions. These shock features are similar to those in S6 L chondrites and indicate that NWA 757 experienced an intense impact event, comparable to the impact event that disrupted the L chondrite parent body at 470 Ma.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Hu, J. and Sharp, T. G. Meteoritics &#038; Planetary Science. doi: 10.1111\/maps.12672 LINK &#8220;Northwest Africa 757 is unique in the LL chondrite group because of its abundant shock-induced melt and high-pressure minerals. Olivine fragments entrained&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[24,7,337,63],"tags":[1816,2869,1807],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/8822"}],"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=8822"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/8822\/revisions"}],"predecessor-version":[{"id":8823,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/8822\/revisions\/8823"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=8822"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=8822"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=8822"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}