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10.1073/pnas.1720619115 http://scihub22266oqcxt.onion/10.1073/pnas.1720619115 C5856551!5856551!29483248     free     free     free Deprecated: Implicit conversion from float 217.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 217.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Proc+Natl+Acad+Sci+U+S+A 2018 ; 115 (11): 2676-80 Nephropedia Template TP {{tp|p=29483248|t=2018. Natural diamond formation by self-redox of ferromagnesian carbonate |pdf=|usr=}}{{29483248}} gab.com Text Natural diamond formation by self-redox of ferromagnesian carbonate JO: Proc Natl Acad Sci U S A http://www.kidney.de/pget.php?&tw=1&pmid=29483248 #FOAvip The presence of extra reducer was thought to be essential for producing natural diamonds from reduction of carbonates. The present study of the Xiuyan meteoritic crater, however, finds natural diamond formation via a subsolidus self-redox of a ferromagnesian carbonate during shock compression to 25?45 GPa and 800?900 °C without melting, fluid, and another reductant. The ability of carbonate to produce diamond by itself implies that diamond would be a very common mineral in the lower mantle where the carbonates are abundant and pressures and temperatures are sufficiently high. Twit Text FOAVip Natural diamond formation by self-redox of ferromagnesian carbonate ????Proc Natl Acad Sci U S A http://www.kidney.de/pget.php?&tw=1&pmid=29483248 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=29483248 #FOAvip English Wikipedia <ref>{{Cite pmid|29483248}}</ref> Natural diamond formation by self-redox of ferromagnesian carbonate #MMPMID29483248 Chen M; Shu J; Xie X; Tan D; Mao Hk Proc Natl Acad Sci U S A 2018[Mar]; 115 (11): 2676-80 PMID29483248show ga The presence of extra reducer was thought to be essential for producing natural diamonds from reduction of carbonates. The present study of the Xiuyan meteoritic crater, however, finds natural diamond formation via a subsolidus self-redox of a ferromagnesian carbonate during shock compression to 25?45 GPa and 800?900 °C without melting, fluid, and another reductant. The ability of carbonate to produce diamond by itself implies that diamond would be a very common mineral in the lower mantle where the carbonates are abundant and pressures and temperatures are sufficiently high. äNatural diamond formation by self-redox of ferromagnesian carbonate (epmc).pdf DeepDyve Pubget Overpricing