Phase transitions and compressibility of NaMgF3 (Neighborite) in perovskite- and post-perovskite-related structures
Monochromatic x‐ray diffraction data collected in‐situ within the diamond anvil cell show perovskite structured Neighborite (NaMgF3) transforms to the CaIrO3‐type post‐perovskite structure between 28 and 30 GPa. Upon laser heating, the CaIrO3‐type structure transforms further to an unknown structure...
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Veröffentlicht in: | Geophysical research letters 2006-06, Vol.33 (11), p.n/a |
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creator | Martin, C. David Crichton, Wilson A. Liu, Haozhe Prakapenka, Vitali Chen, Jiuhua Parise, John B. |
description | Monochromatic x‐ray diffraction data collected in‐situ within the diamond anvil cell show perovskite structured Neighborite (NaMgF3) transforms to the CaIrO3‐type post‐perovskite structure between 28 and 30 GPa. Upon laser heating, the CaIrO3‐type structure transforms further to an unknown structure (Pnnm, designated N‐phase). Upon pressure release, N‐phase NaMgF3 becomes x‐ray amorphous. A structure transformation in post‐perovskite MgSiO3 and MgGeO3 to N‐phase may account for previous observations of extra x‐ray reflections during high pressure experiments and tomographic observations of an additional boundary in the lower mantle below the D″ discontinuity. |
doi_str_mv | 10.1029/2006GL026150 |
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David ; Crichton, Wilson A. ; Liu, Haozhe ; Prakapenka, Vitali ; Chen, Jiuhua ; Parise, John B.</creator><creatorcontrib>Martin, C. David ; Crichton, Wilson A. ; Liu, Haozhe ; Prakapenka, Vitali ; Chen, Jiuhua ; Parise, John B.</creatorcontrib><description>Monochromatic x‐ray diffraction data collected in‐situ within the diamond anvil cell show perovskite structured Neighborite (NaMgF3) transforms to the CaIrO3‐type post‐perovskite structure between 28 and 30 GPa. Upon laser heating, the CaIrO3‐type structure transforms further to an unknown structure (Pnnm, designated N‐phase). Upon pressure release, N‐phase NaMgF3 becomes x‐ray amorphous. 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A structure transformation in post‐perovskite MgSiO3 and MgGeO3 to N‐phase may account for previous observations of extra x‐ray reflections during high pressure experiments and tomographic observations of an additional boundary in the lower mantle below the D″ discontinuity.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNpNkMtOwzAQRS0EEuWx4wO8AcEiMLbTJF7yLEihIARU6sZyUqcY0iR4XKB_j6EIWM3r3JHuJWSHwSEDLo84QDLIgSesDyukx2QcRxlAukp6ADL0PE3WyQbiMwAIEKxH8PZJo6He6Qatt22DVDcTWrazzhlEW9ja-gVtKzrU19MLQfeHxk6fitZZbw6obWhnXPuGL2GMvqVdiz76t3Sm1t5MKHo3L_08fN0ia5Wu0Wz_1E3ycHF-f3oZ5TeDq9PjPLIxMBnpYCfYyr78GJ4JliZFJicCCh5LVphUFhWXlSgnZaWlSYsKJIfACl1BWIpNsrf827n2dW7Qq5nF0tS1bkw7R8WzjPX7LA7g7g-osdR1FcIoLarO2Zl2C8XSEGQsWOD4knu3tVn83UF9xa_-x68GdzkPVQZRtBRZ9ObjV6Tdi0pSkfbVaDhQw_E4PxmNz9Sj-ATYx4nv</recordid><startdate>200606</startdate><enddate>200606</enddate><creator>Martin, C. 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David ; Crichton, Wilson A. ; Liu, Haozhe ; Prakapenka, Vitali ; Chen, Jiuhua ; Parise, John B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-i4019-a20010280261e283176b89d30b2491be79bf29f3cdcfa9e7bf092061e3af0cdc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Martin, C. David</creatorcontrib><creatorcontrib>Crichton, Wilson A.</creatorcontrib><creatorcontrib>Liu, Haozhe</creatorcontrib><creatorcontrib>Prakapenka, Vitali</creatorcontrib><creatorcontrib>Chen, Jiuhua</creatorcontrib><creatorcontrib>Parise, John B.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Martin, C. David</au><au>Crichton, Wilson A.</au><au>Liu, Haozhe</au><au>Prakapenka, Vitali</au><au>Chen, Jiuhua</au><au>Parise, John B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Phase transitions and compressibility of NaMgF3 (Neighborite) in perovskite- and post-perovskite-related structures</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2006-06</date><risdate>2006</risdate><volume>33</volume><issue>11</issue><epage>n/a</epage><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>Monochromatic x‐ray diffraction data collected in‐situ within the diamond anvil cell show perovskite structured Neighborite (NaMgF3) transforms to the CaIrO3‐type post‐perovskite structure between 28 and 30 GPa. Upon laser heating, the CaIrO3‐type structure transforms further to an unknown structure (Pnnm, designated N‐phase). Upon pressure release, N‐phase NaMgF3 becomes x‐ray amorphous. A structure transformation in post‐perovskite MgSiO3 and MgGeO3 to N‐phase may account for previous observations of extra x‐ray reflections during high pressure experiments and tomographic observations of an additional boundary in the lower mantle below the D″ discontinuity.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2006GL026150</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Earth sciences Earth, ocean, space Exact sciences and technology |
title | Phase transitions and compressibility of NaMgF3 (Neighborite) in perovskite- and post-perovskite-related structures |
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