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10.1038/ncomms10679 http://scihub22266oqcxt.onion/10.1038/ncomms10679 C4757754!4757754!26882053     free     free     free Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Nat+Commun 2016 ; 7 (ä): ä Nephropedia Template TP {{tp|p=26882053|t=2016. A potential hidden layer of meteorites below the ice surface of Antarctica |pdf=|usr=}}{{26882053}} gab.com Text A potential hidden layer of meteorites below the ice surface of Antarctica JO: Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=26882053 #FOAvip Antarctica contains some of the most productive regions on Earth for collecting meteorites. These small areas of glacial ice are known as meteorite stranding zones, where upward-flowing ice combines with high ablation rates to concentrate large numbers of englacially transported meteorites onto their surface. However, meteorite collection data shows that iron and stony-iron meteorites are significantly under-represented from these regions as compared with all other sites on Earth. Here we explain how this discrepancy may be due to englacial solar warming, whereby meteorites a few tens of centimetres below the ice surface can be warmed up enough to cause melting of their surrounding ice and sink downwards. We show that meteorites with a high-enough thermal conductivity (for example, iron meteorites) can sink at a rate sufficient to offset the total annual upward ice transport, which may therefore permanently trap them below the ice surface and explain their absence from collection data. Twit Text FOAVip A potential hidden layer of meteorites below the ice surface of Antarctica ????Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=26882053 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=26882053 #FOAvip English Wikipedia <ref>{{Cite pmid|26882053}}</ref> A potential hidden layer of meteorites below the ice surface of Antarctica #MMPMID26882053 Evatt GW; Coughlan MJ; Joy KH; Smedley ARD; Connolly PJ; Abrahams ID Nat Commun 2016[]; 7 (ä): ä PMID26882053show ga Antarctica contains some of the most productive regions on Earth for collecting meteorites. These small areas of glacial ice are known as meteorite stranding zones, where upward-flowing ice combines with high ablation rates to concentrate large numbers of englacially transported meteorites onto their surface. However, meteorite collection data shows that iron and stony-iron meteorites are significantly under-represented from these regions as compared with all other sites on Earth. Here we explain how this discrepancy may be due to englacial solar warming, whereby meteorites a few tens of centimetres below the ice surface can be warmed up enough to cause melting of their surrounding ice and sink downwards. We show that meteorites with a high-enough thermal conductivity (for example, iron meteorites) can sink at a rate sufficient to offset the total annual upward ice transport, which may therefore permanently trap them below the ice surface and explain their absence from collection data. äA potential hidden layer of meteorites below the ice surface of Antarc(epmc).pdf DeepDyve Pubget Overpricing