LINK<\/strong><\/a><\/p>\n“Oxygen three-isotope analysis by secondary ion mass spectrometry of chondrule olivine and pyroxene in combination with electron microprobe analysis were carried out to investigate 24 FeO-poor (type I) and 2 FeO-rich (type II) chondrules from the Kaba (CV) chondrite. The Mg#\u2019s of olivine and pyroxene in individual chondrules are uniform, which confirms that Kaba is one of the least thermally metamorphosed CV3 chondrites. The majority of chondrules in Kaba contain olivine and pyroxene that show indistinguishable \u039417O values (= \u03b417O \u2013 0.52 \u00d7 \u03b418O) within analytical uncertainties, as revealed by multiple spot analyses of individual chondrules. One third of chondrules contain olivine relict grains that are either 16O-rich or 16O-poor relative to other indistinguishable olivine and\/or pyroxene analyses in the same chondrules. Excluding those isotopically recognized relicts, the mean oxygen isotope ratios (\u03b418O, \u03b417O, and \u039417O) of individual chondrules are calculated, which are interpreted to represent those of the final chondrule melt. Most of these isotope ratios plot on or slightly below the primitive chondrule mineral (PCM) line on the oxygen three-isotope diagram, except for the pyroxene-rich type II chondrule that plots above the PCM and on the terrestrial fractionation line. The \u039417O values of type I chondrules range from \u223c \u20138\u2030 to \u223c \u20134\u2030; the pyroxene-rich type II chondrule yields \u223c0\u2030, the olivine-rich type II chondrule \u223c \u20132\u2030. In contrast to the ungrouped carbonaceous chondrite Acfer 094, the Yamato 81020 CO3, and the Allende CV3 chondrite, type I chondrules in Kaba only possess \u039417O values below \u20133\u2030 and a pronounced bimodal distribution of \u039417O values, as evident for those other chondrites, was not observed for Kaba.<\/p>\n
Investigation of the Mg#-\u039417O relationship revealed that \u039417O values tend to increase with decreasing Mg#\u2019s, similar to those observed for CR chondrites though data from Kaba cluster at the high Mg# (>98) and the low \u039417O end (\u20136\u2030 and \u20134\u2030). A mass balance model involving 16O-rich anhydrous dust (\u039417O = \u20138\u2030) and 16O-poor water ice (\u039417O = +2\u2030) in the chondrule precursors suggests that type I chondrules in Kaba would have formed in a moderately high dust enriched protoplanetary disk at relatively dry conditions (\u223c50-100\u00d7 dust enrichment compared to Solar abundance gas and less than 0.6\u00d7 ice enhancement relative to CI chondritic dust). The olivine-rich type II chondrule probably formed in a disk with higher dust enrichment (\u223c2000\u00d7 Solar).”<\/p>\n","protected":false},"excerpt":{"rendered":"
Andreas T. Hertwig, C\u00e9line Defouilloy, Noriko T. Kita Geochimica et Cosmochimica Acta In Press, Accepted Manuscript, Available online 16 December 2017 LINK “Oxygen three-isotope analysis by secondary ion mass spectrometry of chondrule olivine and pyroxene…<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[9,56,148,14,65],"tags":[3273,1839,1864,1812,1636,397],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/14011"}],"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=14011"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/14011\/revisions"}],"predecessor-version":[{"id":14012,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/14011\/revisions\/14012"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=14011"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=14011"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=14011"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}