{"id":4137,"date":"2015-03-19T00:05:19","date_gmt":"2015-03-18T23:05:19","guid":{"rendered":"http:\/\/karmaka.de\/?p=4137"},"modified":"2015-03-19T00:06:07","modified_gmt":"2015-03-18T23:06:07","slug":"various-aspects-of-the-petrogenesis-of-the-martian-shergottite-meteorites","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=4137","title":{"rendered":"Various aspects of the petrogenesis of the Martian shergottite meteorites"},"content":{"rendered":"<p>Jones, J. H. (2015), <\/p>\n<p>Meteoritics &#038; Planetary Science. doi: 10.1111\/maps.12421<\/p>\n<p><a href=\"http:\/\/onlinelibrary.wiley.com\/doi\/10.1111\/maps.12421\/abstract\" target=\"_blank\"><strong>LINK<\/strong><\/a><\/p>\n<div class=\"su-quote su-quote-style-default\"><div class=\"su-quote-inner su-u-clearfix su-u-trim\">Several controversies are associated with the age and origin of the shergottite meteorites, a suite of basaltic samples from Mars. Here, it will be argued that (1) the shergottites have a young igneous age, \u2264600 Myr, (2) their parent magmas were relatively dry, (3) the range of initial isotopic compositions in shergottites is most likely due to assimilation of crustal materials by mantle-derived basaltic magmas, and (4) the intercumulus liquid compositions of shergottites such as Shergotty and Zagami are relatively well constrained.<\/div><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Jones, J. H. (2015), Meteoritics &#038; Planetary Science. doi: 10.1111\/maps.12421 LINK<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[42,43],"tags":[1828,246,1829,697,1142],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/4137"}],"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=4137"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/4137\/revisions"}],"predecessor-version":[{"id":4138,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/4137\/revisions\/4138"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=4137"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=4137"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=4137"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}