{"id":12552,"date":"2017-05-26T20:01:00","date_gmt":"2017-05-26T18:01:00","guid":{"rendered":"http:\/\/karmaka.de\/?p=12552"},"modified":"2017-05-26T20:01:00","modified_gmt":"2017-05-26T18:01:00","slug":"silicate-sio-reaction-in-a-protoplanetary-disk-recorded-by-oxygen-isotopes-in-chondrules","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=12552","title":{"rendered":"Silicate\u2013SiO reaction in a protoplanetary disk recorded by oxygen isotopes in chondrules"},"content":{"rendered":"<p>Ryoji Tanaka &#038; Eizo Nakamura<\/p>\n<p>Nature Astronomy 1,<br \/>\nArticle number: 0137 (2017)<br \/>\ndoi:10.1038\/s41550-017-0137<\/p>\n<p><a href=\"https:\/\/www.nature.com\/articles\/s41550-017-0137\" target=\"_blank\"><strong>LINK<\/strong><\/a><\/p>\n<p>&#8220;The formation of planetesimals and planetary embryos during the earliest stages of the solar protoplanetary disk largely determined the composition and structure of the terrestrial planets. Within a few million years of the birth of the Solar System, chondrule formation and the accretion of the parent bodies of differentiated achondrites and the terrestrial planets took place in the inner protoplanetary disk 1,2 . Here we show that, for chondrules in unequilibrated enstatite chondrites, high-precision \u039417O values (where \u039417O is the deviation of the \u03b417O value from a terrestrial silicate fractionation line) vary significantly (ranging from \u22120.49 to +0.84\u2030) and fall on an array with a steep slope of 1.27 on a three-oxygen-isotope plot. This array can be explained by the reaction between an olivine-rich chondrule melt and an SiO-rich gas derived from vaporized dust and nebular gas. Our study suggests that a large proportion of the building blocks of planetary embryos formed by successive silicate\u2013gas interaction processes: silicate\u2013H2O followed by silicate\u2013SiO interactions under more oxidized and reduced conditions, respectively, within a few million years of the formation of the Solar System.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Ryoji Tanaka &#038; Eizo Nakamura Nature Astronomy 1, Article number: 0137 (2017) doi:10.1038\/s41550-017-0137 LINK &#8220;The formation of planetesimals and planetary embryos during the earliest stages of the solar protoplanetary disk largely determined the composition and&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[56,72,17,65,71],"tags":[1813,2959,397,3875,3876],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/12552"}],"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=12552"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/12552\/revisions"}],"predecessor-version":[{"id":12553,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/12552\/revisions\/12553"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=12552"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=12552"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=12552"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}