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Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites
This paper presents the results of a Raman spectroscopic study of shock melt veins in L6 chondritic meteorites Dhofar 717 and 864, and conclusions about the P–T parameters recorded in these meteorites after the impact event. The primary minerals of the host chondrite include olivine, orthopyroxene,...
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Published in: | Doklady earth sciences 2019-03, Vol.485 (1), p.327-330 |
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description | This paper presents the results of a Raman spectroscopic study of shock melt veins in L6 chondritic meteorites Dhofar 717 and 864, and conclusions about the
P–T
parameters recorded in these meteorites after the impact event. The primary minerals of the host chondrite include olivine, orthopyroxene, clinopyroxene, plagioclase, chromite, phosphates, troilite, and kamasite. Shock melt veins up to 1 cm thick contain fragments of the high-pressure minerals ringwoodite, wadsleyite, majorite, akimotoite, jadeite, lingunite, and tuite and quenched melt consisting of majorite, ringwoodite, troilite, and kamasite. The mineral associations of the Dhofar 717 and 864 chondrites indicate high peak
PT
parameters of the impact in the region of stability of majorite (>20 GPa and >2500 K) and bridgmanite (>25 GPa and >2500 K). The presence of lingunite also directly indicates a peak pressure in the area of stability of the bridgmanite. |
doi_str_mv | 10.1134/S1028334X19030322 |
format | article |
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P–T
parameters recorded in these meteorites after the impact event. The primary minerals of the host chondrite include olivine, orthopyroxene, clinopyroxene, plagioclase, chromite, phosphates, troilite, and kamasite. Shock melt veins up to 1 cm thick contain fragments of the high-pressure minerals ringwoodite, wadsleyite, majorite, akimotoite, jadeite, lingunite, and tuite and quenched melt consisting of majorite, ringwoodite, troilite, and kamasite. The mineral associations of the Dhofar 717 and 864 chondrites indicate high peak
PT
parameters of the impact in the region of stability of majorite (>20 GPa and >2500 K) and bridgmanite (>25 GPa and >2500 K). The presence of lingunite also directly indicates a peak pressure in the area of stability of the bridgmanite.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X19030322</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Chondrites ; Chromite ; Earth and Environmental Science ; Earth Sciences ; Geochemistry ; High pressure ; Jadeite ; Meteorites ; Meteors & meteorites ; Minerals ; Olivine ; Parameters ; Peak pressure ; Phosphates ; Plagioclase ; Pressure ; Raman spectroscopy ; Spinel group ; Stability ; Troilite</subject><ispartof>Doklady earth sciences, 2019-03, Vol.485 (1), p.327-330</ispartof><rights>Pleiades Publishing, Ltd. 2019</rights><rights>COPYRIGHT 2019 Springer</rights><rights>Copyright Springer Nature B.V. 2019</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c421t-a945dee7ed18a5c597c27b4506dde642bcaa8c789e5705e0ca177433a65ec61d3</citedby><cites>FETCH-LOGICAL-c421t-a945dee7ed18a5c597c27b4506dde642bcaa8c789e5705e0ca177433a65ec61d3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,786,790,27957,27958</link.rule.ids></links><search><creatorcontrib>Litasov, K. D.</creatorcontrib><creatorcontrib>Badyukov, D. D.</creatorcontrib><creatorcontrib>Pokhilenko, N. P.</creatorcontrib><title>Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites</title><title>Doklady earth sciences</title><addtitle>Dokl. Earth Sc</addtitle><description>This paper presents the results of a Raman spectroscopic study of shock melt veins in L6 chondritic meteorites Dhofar 717 and 864, and conclusions about the
P–T
parameters recorded in these meteorites after the impact event. The primary minerals of the host chondrite include olivine, orthopyroxene, clinopyroxene, plagioclase, chromite, phosphates, troilite, and kamasite. Shock melt veins up to 1 cm thick contain fragments of the high-pressure minerals ringwoodite, wadsleyite, majorite, akimotoite, jadeite, lingunite, and tuite and quenched melt consisting of majorite, ringwoodite, troilite, and kamasite. The mineral associations of the Dhofar 717 and 864 chondrites indicate high peak
PT
parameters of the impact in the region of stability of majorite (>20 GPa and >2500 K) and bridgmanite (>25 GPa and >2500 K). The presence of lingunite also directly indicates a peak pressure in the area of stability of the bridgmanite.</description><subject>Chondrites</subject><subject>Chromite</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>High pressure</subject><subject>Jadeite</subject><subject>Meteorites</subject><subject>Meteors & meteorites</subject><subject>Minerals</subject><subject>Olivine</subject><subject>Parameters</subject><subject>Peak pressure</subject><subject>Phosphates</subject><subject>Plagioclase</subject><subject>Pressure</subject><subject>Raman spectroscopy</subject><subject>Spinel group</subject><subject>Stability</subject><subject>Troilite</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp1kE1LAzEQhhdRsFZ_gLeA56353GSPpVorVCyo4EWWNDvbTekmNdke_PemrOBBZA4zzLzPfGXZNcETQhi_fSGYKsb4Oykxw4zSk2xEBCO5YoKfpjiV82P9PLuIcYsx51yUo-xj7kOne-sdWumgO-ghROQbtLCbNl8FiPEQAD1ZB0HvIrIO9S2gu9Y3OiBJJNKuRqrgaNZ6VwfbJ3Fq4o9RvMzOmkTB1Y8fZ2_z-9fZIl8-PzzOpsvccEr6XJdc1AASaqK0MKKUhso1F7ioayg4XRutlZGqBCGxAGw0kZIzpgsBpiA1G2c3Q9998J8HiH219Yfg0siKUkbSpaookmoyqDZ6B5V1je-DNslq6KzxDhqb8lOh0hBWcpUAMgAm-BgDNNU-2E6Hr4rg6vj26s_bE0MHJiat20D4XeV_6BuodoLH</recordid><startdate>20190301</startdate><enddate>20190301</enddate><creator>Litasov, K. D.</creator><creator>Badyukov, D. D.</creator><creator>Pokhilenko, N. P.</creator><general>Pleiades Publishing</general><general>Springer</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20190301</creationdate><title>Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites</title><author>Litasov, K. D. ; Badyukov, D. D. ; Pokhilenko, N. P.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c421t-a945dee7ed18a5c597c27b4506dde642bcaa8c789e5705e0ca177433a65ec61d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Chondrites</topic><topic>Chromite</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geochemistry</topic><topic>High pressure</topic><topic>Jadeite</topic><topic>Meteorites</topic><topic>Meteors & meteorites</topic><topic>Minerals</topic><topic>Olivine</topic><topic>Parameters</topic><topic>Peak pressure</topic><topic>Phosphates</topic><topic>Plagioclase</topic><topic>Pressure</topic><topic>Raman spectroscopy</topic><topic>Spinel group</topic><topic>Stability</topic><topic>Troilite</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Litasov, K. D.</creatorcontrib><creatorcontrib>Badyukov, D. D.</creatorcontrib><creatorcontrib>Pokhilenko, N. P.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Doklady earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Litasov, K. D.</au><au>Badyukov, D. D.</au><au>Pokhilenko, N. P.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2019-03-01</date><risdate>2019</risdate><volume>485</volume><issue>1</issue><spage>327</spage><epage>330</epage><pages>327-330</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>This paper presents the results of a Raman spectroscopic study of shock melt veins in L6 chondritic meteorites Dhofar 717 and 864, and conclusions about the
P–T
parameters recorded in these meteorites after the impact event. The primary minerals of the host chondrite include olivine, orthopyroxene, clinopyroxene, plagioclase, chromite, phosphates, troilite, and kamasite. Shock melt veins up to 1 cm thick contain fragments of the high-pressure minerals ringwoodite, wadsleyite, majorite, akimotoite, jadeite, lingunite, and tuite and quenched melt consisting of majorite, ringwoodite, troilite, and kamasite. The mineral associations of the Dhofar 717 and 864 chondrites indicate high peak
PT
parameters of the impact in the region of stability of majorite (>20 GPa and >2500 K) and bridgmanite (>25 GPa and >2500 K). The presence of lingunite also directly indicates a peak pressure in the area of stability of the bridgmanite.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1028334X19030322</doi><tpages>4</tpages></addata></record> |
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subjects | Chondrites Chromite Earth and Environmental Science Earth Sciences Geochemistry High pressure Jadeite Meteorites Meteors & meteorites Minerals Olivine Parameters Peak pressure Phosphates Plagioclase Pressure Raman spectroscopy Spinel group Stability Troilite |
title | Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites |
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