{"id":2070,"date":"2014-11-11T15:59:45","date_gmt":"2014-11-11T14:59:45","guid":{"rendered":"http:\/\/karmaka.de\/?page_id=2070"},"modified":"2016-05-16T19:53:22","modified_gmt":"2016-05-16T17:53:22","slug":"csatalja","status":"publish","type":"page","link":"https:\/\/karmaka.de\/?page_id=2070","title":{"rendered":"Cs\u00e1talja"},"content":{"rendered":"<div class=\"su-spacer\" style=\"height:10px\"><\/div>\n<p style=\"text-align: center;\"><strong><span style=\"font-size: 24pt;\">CS\u00c1TALJA<\/span><\/strong><\/p>\n<p>UPDATE (24 February 2015):  <\/p>\n<p><a href=\"http:\/\/www.lpi.usra.edu\/meteor\/metbull.php?sea=Csatalja&#038;sfor=names&#038;ants=&#038;falls=&#038;valids=&#038;stype=contains&#038;lrec=50&#038;map=ge&#038;browse=&#038;country=All&#038;srt=name&#038;categ=All&#038;mblist=All&#038;rect=&#038;phot=&#038;snew=0&#038;pnt=Normal%20table&#038;code=61584\" target=\"_blank\"><strong>Entry in the Meteoritical Bulletin (23 February 2015)<\/strong><\/a><\/p>\n<p><a href=\"http:\/\/www.sciencedirect.com\/science\/article\/pii\/S0032063314003456\" target=\"_blank\"><strong>Cs\u00e1talja, the largest H4-5 chondrite from Hungary<\/strong><\/a><\/p>\n<p>Planetary and Space Science<br \/>\navailable online 18 November 2014<\/p>\n<p>J\u00e1nos Kov\u00e1cs, Istv\u00e1n Saj\u00f3, Zsuzsanna M\u00e1rton, Viktor J\u00e1ger, Tibor Heged\u00fcs, Tibor Berecz, Tam\u00e1s T\u00f3th, P\u00e9ter Gyenizse, Andr\u00e1s Podobni<\/p>\n<div class=\"su-quote su-quote-style-default\"><div class=\"su-quote-inner su-u-clearfix su-u-trim\">We report here for the first time the composition and mineralogical studies on a new meteorite, which was found in August 2012 near the village of Cs\u00e1talja, Hungary (46 \u00b00\u201921\u201dN; 18 \u00b059\u201927\u201dE). The Cs\u00e1talja meteorite is classified as a H4-5 ordinary chondrite with shock stage S2 and a degree of weathering W1 and the total mass is 15 kg. The Cs\u00e1talja meteorite is characterized by well-defined chondrules composed either of olivine or pyroxene. X-ray diffractogram shows the primary phases olivine, pyroxene, kamacite, and albite. Metal particles were extracted from the bulk powdered samples exhibit only kamacite and small amounts of the intergrowth taenite\/kamacite. Raman spectra of forsterite indicate that Cs\u00e1talja meteorite was suffered under relatively low shock pressure regime, respectively. The texture of chondrules varies from nonporphyritic (e.g., barred olivine, radial pyroxene) to porphyritic ones (e.g., granular olivine as well as olivine pyroxene). The meteorite name has not yet approved by the Nomenclature Committee of the Meteoritical Society.<\/div><\/div>\n<div id=\"attachment_2268\" style=\"width: 1010px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-Hauptmasse.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-2268\" class=\"wp-image-2268 size-full\" src=\"http:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-Hauptmasse.jpg\" alt=\"main mass\" width=\"1000\" height=\"750\" srcset=\"https:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-Hauptmasse.jpg 1000w, https:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-Hauptmasse-300x225.jpg 300w\" sizes=\"(max-width: 1000px) 100vw, 1000px\" \/><\/a><p id=\"caption-attachment-2268\" class=\"wp-caption-text\">Cs\u00e1talja main mass , image credit: Zsolt Kereszty<\/p><\/div>\n<div id=\"attachment_3905\" style=\"width: 906px\" class=\"wp-caption alignnone\"><a href=\"http:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-k.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3905\" src=\"http:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-k.jpg\" alt=\"Cs\u00e1talja find location: 46.006\u00b0 N, 18.991\u00b0 E\" width=\"896\" height=\"660\" class=\"size-full wp-image-3905\" srcset=\"https:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-k.jpg 896w, https:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-k-300x220.jpg 300w\" sizes=\"(max-width: 896px) 100vw, 896px\" \/><\/a><p id=\"caption-attachment-3905\" class=\"wp-caption-text\">Cs\u00e1talja find location: 46.006\u00b0 N, 18.991\u00b0 E<\/p><\/div>\n<div id=\"attachment_3907\" style=\"width: 1510px\" class=\"wp-caption alignnone\"><a href=\"http:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-find-location.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-3907\" src=\"http:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-find-location.jpg\" alt=\"Exact find location \/ Photo: Zsolt Kereszty\" width=\"1500\" height=\"1000\" class=\"size-full wp-image-3907\" srcset=\"https:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-find-location.jpg 1500w, https:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-find-location-300x200.jpg 300w, https:\/\/karmaka.de\/wp-content\/uploads\/2014\/11\/Csatalja-find-location-1024x682.jpg 1024w\" sizes=\"(max-width: 1500px) 100vw, 1500px\" \/><\/a><p id=\"caption-attachment-3907\" class=\"wp-caption-text\">Exact find location \/ Photo: Zsolt Kereszty<\/p><\/div>\n<p><span style=\"font-size: 12pt;\"><strong>UNDER CONSTRUCTION<\/strong><\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>CS\u00c1TALJA UPDATE (24 February 2015): Entry in the Meteoritical Bulletin (23 February 2015) Cs\u00e1talja, the largest H4-5 chondrite from Hungary Planetary and Space Science available online 18 November 2014 J\u00e1nos Kov\u00e1cs, Istv\u00e1n Saj\u00f3, Zsuzsanna M\u00e1rton,&#8230;<\/p>\n","protected":false},"author":1,"featured_media":2268,"parent":64,"menu_order":0,"comment_status":"open","ping_status":"open","template":"page-template-wide.php","meta":{"footnotes":""},"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/pages\/2070"}],"collection":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/types\/page"}],"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=2070"}],"version-history":[{"count":13,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/pages\/2070\/revisions"}],"predecessor-version":[{"id":8741,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/pages\/2070\/revisions\/8741"}],"up":[{"embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/pages\/64"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/media\/2268"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=2070"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}