{"id":14166,"date":"2018-01-31T15:19:21","date_gmt":"2018-01-31T14:19:21","guid":{"rendered":"http:\/\/karmaka.de\/?p=14166"},"modified":"2018-01-31T15:21:21","modified_gmt":"2018-01-31T14:21:21","slug":"multiple-sulfur-isotopic-composition-of-main-group-pallasites-support-genetic-links-to-iiiab-iron-meteorites","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=14166","title":{"rendered":"Multiple Sulfur Isotopic Composition of Main Group Pallasites Support Genetic Links to IIIAB Iron Meteorites"},"content":{"rendered":"<p>James W. Dottin III, James Farquhar, Jabrane Labidi<\/p>\n<p>Geochimica et Cosmochimica Acta<br \/>\nIn Press, Accepted Manuscript, Available online 31 January 2018<\/p>\n<p><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0016703718300164\" target=\"_blank\"><strong>LINK<\/strong><\/a><\/p>\n<p>&#8220;This study reports the quadruple sulfur isotope composition of troilite nodules from Main Group Pallasites. Values range from -0.23\u2030 to 0.34\u2030 (average = 0.03\u00b10.17\u2030 S.D.) in \u03b434S and 0.008\u2030 to 0.025\u2030 (average = 0.018\u00b1 0.006\u2030 S.D.) in \u039433S and -0.38 to -0.01 (average = -0.17\u00b10.11\u2030 S.D.) in \u039436S. The variance of these analyses is comparable to estimates of analytical uncertainty (\u00b10.3\u2030, \u00b1 0.008\u2030, and \u00b10.3\u2030, for \u03b434S, \u039433S, and \u039436S, respectively) and the average of these values is taken as a constraint on the composition of sulfur in the MG Pallasite parent body. The different \u039433S value compared to CDT and IAB iron meteorites at a similar \u03b434S value is interpreted as a mass-independent signature. This signature is similar in magnitude and direction to previously published values observed in IIIAB iron meteorites, further supporting a genetic relationship between the two groups of meteorites.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>James W. Dottin III, James Farquhar, Jabrane Labidi Geochimica et Cosmochimica Acta In Press, Accepted Manuscript, Available online 31 January 2018 LINK &#8220;This study reports the quadruple sulfur isotope composition of troilite nodules from Main&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1038,214,2583,810],"tags":[1541,1874,2585,812,2118,3327],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/14166"}],"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=14166"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/14166\/revisions"}],"predecessor-version":[{"id":14167,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/14166\/revisions\/14167"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=14166"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=14166"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=14166"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}