{"id":22943,"date":"2020-08-03T12:21:04","date_gmt":"2020-08-03T10:21:04","guid":{"rendered":"http:\/\/karmaka.de\/?p=22943"},"modified":"2020-08-03T13:06:55","modified_gmt":"2020-08-03T11:06:55","slug":"sierra-gorda-009-a-new-member-of-the-metal%e2%80%90rich-g-chondrites-grouplet","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=22943","title":{"rendered":"Sierra Gorda 009: A new member of the metal\u2010rich G chondrites grouplet"},"content":{"rendered":"\n<p>Marina A. Ivanova, Cyril A. Lorenz, Munir Humayun, Catherine M. Corrigan, Thomas Ludwig, Mario Trieloff, Kevin Righter, Ian A. Franchi, Alexander B. Verchovsky, Ekaterina V. Korochantseva, Vladimir V. Kozlov, Svetlana N. Teplyakova, Alexander V. Korochantsev, Victor I. Grokhovsky<\/p>\n\n\n\n<p>Meteoritics &amp; Planetary Science<br>Version of Record online: 03 August 2020<\/p>\n\n\n\n<p><a href=\"https:\/\/onlinelibrary.wiley.com\/doi\/10.1111\/maps.13546\" target=\"_blank\" rel=\"noreferrer noopener\"><strong>LINK<\/strong><\/a><\/p>\n\n\n\n<p class=\"justify-text\">&#8220;We investigated the metal\u2010rich chondrite Sierra Gorda (SG) 009, a member of the new G chondrite grouplet (also including NWA 5492, GRO 95551). G chondrites contain 23% metal, very reduced silicates, and rare oxidized mineral phases (Mg\u2010chromite, FeO\u2010rich pyroxene). G chondrites are not related to CH\u2010CB chondrites, based on bulk O, C, and N isotopic compositions, mineralogy, and geochemistry. G chondrites have no fine\u2010grained matrix or matrix lumps enclosing hydrated material typical for CH\u2010CB chondrites. G chondrites\u2019 average metal compositions are similar to H chondrites. Siderophile and lithophile geochemistry indicates sulfidization and fractionation of the SG 009 metal and silicates, unlike NWA 5492 and GRO 95551. The G chondrites have average O isotopic compositions \u039417O&gt;0\u2030 ranging between bulk enstatite (E) and ordinary (O) chondrites. An Al\u2010rich chondrule from SG 009 has \u039417O&gt;0\u2030 indicating some heterogeneity in oxygen isotopic composition of G chondrite components. SG 009\u2019s bulk carbon and nitrogen isotopic compositions correspond to E and O chondrites. Neon isotopic composition reflects a mixture of cosmogenic and solar components, and cosmic ray exposure age of SG 009 is typical for O, E, and R chondrites. G chondrites are closely related to O, E, and R chondrites and may represent a unique metal\u2010rich parent asteroid containing primitive and fractionated material from the inner solar system. Oxidizing and reducing conditions during SG 009 formation may be connected with a chemical microenvironment and possibly could indicate that G chondrites may have formed by a planetesimal collision resulting in the lack of matrix.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Marina A. Ivanova, Cyril A. Lorenz, Munir Humayun, Catherine M. Corrigan, Thomas Ludwig, Mario Trieloff, Kevin Righter, Ian A. Franchi, Alexander B. Verchovsky, Ekaterina V. Korochantseva, Vladimir V. Kozlov, Svetlana N. Teplyakova, Alexander V. Korochantsev,&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[59,69,4835,65],"tags":[1817,1813,4831,1729,2373,4830,4839,5634,1728,1807,2163,3129,5055],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/22943"}],"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=22943"}],"version-history":[{"count":3,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/22943\/revisions"}],"predecessor-version":[{"id":22946,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/22943\/revisions\/22946"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=22943"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=22943"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=22943"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}