Shrilankite Inclusions in Garnets from Kimberlite Bodies and Diamondiferous Volcanic–Sedimentary Rocks of the Yakutian Kimberlite Province, Russia
Pyrope–almandine garnets (Mg# = 28.3–44.9, Ca# = 15.5–21.3) from a heavy mineral concentrate of diamondiferous kimberlites of the largest diamond deposit, the Yubileinaya pipe, along with kimberlite- like rocks and diamondiferous volcano–sediments of the Laptev Sea coast, have been found to contain...
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creator | Biller, A. Ya Logvinova, A. M. Babushkina, S. A. Oleynikov, O. B. Sobolev, N. V. |
description | Pyrope–almandine garnets (Mg# = 28.3–44.9, Ca# = 15.5–21.3) from a heavy mineral concentrate of diamondiferous kimberlites of the largest diamond deposit, the Yubileinaya pipe, along with kimberlite- like rocks and diamondiferous volcano–sediments of the Laptev Sea coast, have been found to contain polymineral, predominantly acicular inclusions, composed of aggregates of shrilankite (Ti
2
ZrO
6
), rutile, ilmenite, clinopyroxene, and apatite. The presence of shrilankite as an inclusion in garnets from assumed garnet–pyroxene rocks of the lower crust, lifted up by diamond-bearing kimberlite, allows it to be considered as an indicator mineral of kimberlite, which expands the possibilities when searching for kimberlite in the Arctic. |
doi_str_mv | 10.1134/S1028334X18010117 |
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2
ZrO
6
), rutile, ilmenite, clinopyroxene, and apatite. The presence of shrilankite as an inclusion in garnets from assumed garnet–pyroxene rocks of the lower crust, lifted up by diamond-bearing kimberlite, allows it to be considered as an indicator mineral of kimberlite, which expands the possibilities when searching for kimberlite in the Arctic.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X18010117</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Apatite ; Diamonds ; Earth and Environmental Science ; Earth Sciences ; Garnet ; Garnets ; Geology ; Ilmenite ; Inclusions ; Kimberlite ; Kimberlites ; Magnesium aluminum silicates ; Minerals ; Phosphate minerals ; Provinces ; Pyroxenes ; Rock ; Rutile ; Sedimentary rocks ; Sediments ; Sediments (Geology) ; Volcanic activity ; Volcanoes</subject><ispartof>Doklady earth sciences, 2018, Vol.478 (1), p.15-19</ispartof><rights>Pleiades Publishing, Ltd. 2018</rights><rights>COPYRIGHT 2018 Springer</rights><rights>Doklady Earth Sciences is a copyright of Springer, (2018). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c355t-e16728fff4642c8efc7a89aae6918063eed49150db299a8716161d9f7b1e715a3</citedby><cites>FETCH-LOGICAL-c355t-e16728fff4642c8efc7a89aae6918063eed49150db299a8716161d9f7b1e715a3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1028334X18010117$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1028334X18010117$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Biller, A. Ya</creatorcontrib><creatorcontrib>Logvinova, A. M.</creatorcontrib><creatorcontrib>Babushkina, S. A.</creatorcontrib><creatorcontrib>Oleynikov, O. B.</creatorcontrib><creatorcontrib>Sobolev, N. V.</creatorcontrib><title>Shrilankite Inclusions in Garnets from Kimberlite Bodies and Diamondiferous Volcanic–Sedimentary Rocks of the Yakutian Kimberlite Province, Russia</title><title>Doklady earth sciences</title><addtitle>Dokl. Earth Sc</addtitle><description>Pyrope–almandine garnets (Mg# = 28.3–44.9, Ca# = 15.5–21.3) from a heavy mineral concentrate of diamondiferous kimberlites of the largest diamond deposit, the Yubileinaya pipe, along with kimberlite- like rocks and diamondiferous volcano–sediments of the Laptev Sea coast, have been found to contain polymineral, predominantly acicular inclusions, composed of aggregates of shrilankite (Ti
2
ZrO
6
), rutile, ilmenite, clinopyroxene, and apatite. The presence of shrilankite as an inclusion in garnets from assumed garnet–pyroxene rocks of the lower crust, lifted up by diamond-bearing kimberlite, allows it to be considered as an indicator mineral of kimberlite, which expands the possibilities when searching for kimberlite in the Arctic.</description><subject>Apatite</subject><subject>Diamonds</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Garnet</subject><subject>Garnets</subject><subject>Geology</subject><subject>Ilmenite</subject><subject>Inclusions</subject><subject>Kimberlite</subject><subject>Kimberlites</subject><subject>Magnesium aluminum silicates</subject><subject>Minerals</subject><subject>Phosphate minerals</subject><subject>Provinces</subject><subject>Pyroxenes</subject><subject>Rock</subject><subject>Rutile</subject><subject>Sedimentary rocks</subject><subject>Sediments</subject><subject>Sediments (Geology)</subject><subject>Volcanic activity</subject><subject>Volcanoes</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kdFO3TAMhiu0SWOMB-Au0m5XFjdJm14ytjE0JBBnTOOqykkdMKdNIGkn7W7vMJ5wT0KOziSQ0OQLW_b_2ZZdFHvA9wGEfL8AXmkh5A_QHDhAs1VsgxJQaqHkixzncrmuvypep3TDuZRStdvF_eI60mD8iiZkx94Oc6LgEyPPjkz0OCXmYhjZVxqXGIe16kPoCRMzvmcfyYzB9-Qwhjmx72GwxpP9-_vPAnsa0U8m_mLnwa4SC45N18guzWqeyPinHc9i-Ene4jt2PqdE5k3x0pkh4e4_v1NcfP707fBLeXJ6dHx4cFJaodRUItRNpZ1zspaV1ehsY3RrDNZtvkItEHvZguL9smpboxuos_Wta5aADSgjdoq3m763MdzNmKbuJszR55FdxbnmSlZSZtX-RnVlBuzIuzBFY7P1OJINHh3l_IESXNaN0JAB2AA2hpQiuu420pgv0QHv1t_qnn0rM9WGSVnrrzA-rvJ_6AFhQZm0</recordid><startdate>2018</startdate><enddate>2018</enddate><creator>Biller, A. Ya</creator><creator>Logvinova, A. M.</creator><creator>Babushkina, S. A.</creator><creator>Oleynikov, O. B.</creator><creator>Sobolev, N. 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M. ; Babushkina, S. A. ; Oleynikov, O. B. ; Sobolev, N. V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c355t-e16728fff4642c8efc7a89aae6918063eed49150db299a8716161d9f7b1e715a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Apatite</topic><topic>Diamonds</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Garnet</topic><topic>Garnets</topic><topic>Geology</topic><topic>Ilmenite</topic><topic>Inclusions</topic><topic>Kimberlite</topic><topic>Kimberlites</topic><topic>Magnesium aluminum silicates</topic><topic>Minerals</topic><topic>Phosphate minerals</topic><topic>Provinces</topic><topic>Pyroxenes</topic><topic>Rock</topic><topic>Rutile</topic><topic>Sedimentary rocks</topic><topic>Sediments</topic><topic>Sediments (Geology)</topic><topic>Volcanic activity</topic><topic>Volcanoes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Biller, A. 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Ya</au><au>Logvinova, A. M.</au><au>Babushkina, S. A.</au><au>Oleynikov, O. B.</au><au>Sobolev, N. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Shrilankite Inclusions in Garnets from Kimberlite Bodies and Diamondiferous Volcanic–Sedimentary Rocks of the Yakutian Kimberlite Province, Russia</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2018</date><risdate>2018</risdate><volume>478</volume><issue>1</issue><spage>15</spage><epage>19</epage><pages>15-19</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>Pyrope–almandine garnets (Mg# = 28.3–44.9, Ca# = 15.5–21.3) from a heavy mineral concentrate of diamondiferous kimberlites of the largest diamond deposit, the Yubileinaya pipe, along with kimberlite- like rocks and diamondiferous volcano–sediments of the Laptev Sea coast, have been found to contain polymineral, predominantly acicular inclusions, composed of aggregates of shrilankite (Ti
2
ZrO
6
), rutile, ilmenite, clinopyroxene, and apatite. The presence of shrilankite as an inclusion in garnets from assumed garnet–pyroxene rocks of the lower crust, lifted up by diamond-bearing kimberlite, allows it to be considered as an indicator mineral of kimberlite, which expands the possibilities when searching for kimberlite in the Arctic.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1028334X18010117</doi><tpages>5</tpages></addata></record> |
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subjects | Apatite Diamonds Earth and Environmental Science Earth Sciences Garnet Garnets Geology Ilmenite Inclusions Kimberlite Kimberlites Magnesium aluminum silicates Minerals Phosphate minerals Provinces Pyroxenes Rock Rutile Sedimentary rocks Sediments Sediments (Geology) Volcanic activity Volcanoes |
title | Shrilankite Inclusions in Garnets from Kimberlite Bodies and Diamondiferous Volcanic–Sedimentary Rocks of the Yakutian Kimberlite Province, Russia |
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