Formation of eudialyte-bearing phonolite from Kontozero carbonatite paleovolcano, Kola Peninsula
The results of the geological and petrologic study of eudialyte-bearing phonolite from the Late Devonian Kontozero carbonatite paleovolcano are discussed in the paper. This eudialyte-bearing phonolite corresponds to the primary melt derived from the metasomatized upper mantle source composed of phlo...
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| Veröffentlicht in: | Geology of ore deposits 2012-12, Vol.54 (7), p.540-556 |
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| creator | Petrovsky, M. N. Savchenko, E. A. Kalachev, V. Yu |
| description | The results of the geological and petrologic study of eudialyte-bearing phonolite from the Late Devonian Kontozero carbonatite paleovolcano are discussed in the paper. This eudialyte-bearing phonolite corresponds to the primary melt derived from the metasomatized upper mantle source composed of phlogopite-amphibole eclogite. The average ZrO
2
content in the Kontozero phonolite (1.02 wt %) is considered to be cotectic (Kogarko et al., 1988). Similar REE patterns of the Kontozero eudialyte-bearing phonolite and porphyritic lujavrite from the chilled contact zone of the Lovozero eudyalite complex and close REE and Zr concentrations in the compared rocks show that this complex could have been formed from a melt similar in composition to the phonolite melt of Kontozero. |
| doi_str_mv | 10.1134/S1075701512070057 |
| format | Article |
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2
content in the Kontozero phonolite (1.02 wt %) is considered to be cotectic (Kogarko et al., 1988). Similar REE patterns of the Kontozero eudialyte-bearing phonolite and porphyritic lujavrite from the chilled contact zone of the Lovozero eudyalite complex and close REE and Zr concentrations in the compared rocks show that this complex could have been formed from a melt similar in composition to the phonolite melt of Kontozero.</description><identifier>ISSN: 1075-7015</identifier><identifier>EISSN: 1555-6476</identifier><identifier>DOI: 10.1134/S1075701512070057</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Mineral Resources</subject><ispartof>Geology of ore deposits, 2012-12, Vol.54 (7), p.540-556</ispartof><rights>Pleiades Publishing, Ltd. 2012</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a311t-824e51f6a2bad7c712f82c9156c913aa20503f34ba7a6ce58fd23f261a2064a73</citedby><cites>FETCH-LOGICAL-a311t-824e51f6a2bad7c712f82c9156c913aa20503f34ba7a6ce58fd23f261a2064a73</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/S1075701512070057$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1075701512070057$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Petrovsky, M. N.</creatorcontrib><creatorcontrib>Savchenko, E. A.</creatorcontrib><creatorcontrib>Kalachev, V. Yu</creatorcontrib><title>Formation of eudialyte-bearing phonolite from Kontozero carbonatite paleovolcano, Kola Peninsula</title><title>Geology of ore deposits</title><addtitle>Geol. Ore Deposits</addtitle><description>The results of the geological and petrologic study of eudialyte-bearing phonolite from the Late Devonian Kontozero carbonatite paleovolcano are discussed in the paper. This eudialyte-bearing phonolite corresponds to the primary melt derived from the metasomatized upper mantle source composed of phlogopite-amphibole eclogite. The average ZrO
2
content in the Kontozero phonolite (1.02 wt %) is considered to be cotectic (Kogarko et al., 1988). Similar REE patterns of the Kontozero eudialyte-bearing phonolite and porphyritic lujavrite from the chilled contact zone of the Lovozero eudyalite complex and close REE and Zr concentrations in the compared rocks show that this complex could have been formed from a melt similar in composition to the phonolite melt of Kontozero.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Mineral Resources</subject><issn>1075-7015</issn><issn>1555-6476</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNp9kFFLAzEMgIsoOKc_wLf7AZ427bWdjzKcigMF9fnM3bV6o2uO9ibMX2_HfBN8SQJfvpCEsXPglwCyunoBbpThoEBww7kyB2wCSqlSV0Yf5jrjcseP2UlKK84rJThM2PuC4hrHnkJBrrCbrke_HW3ZWIx9-CiGTwrk-9EWLtK6eKQw0reNVLQYGwrZzGhAb-mLfIuBLnKPx-LZhj6kjcdTduTQJ3v2m6fsbXH7Or8vl093D_ObZYkSYCxnorIKnEbRYGdaA8LNRHsNSucgEQVXXDpZNWhQt1bNXCekExoy0RUaOWWwn9tGSilaVw-xX2Pc1sDr3YvqPy_Kjtg7adgda2O9ok0Mec1_pB_piGmw</recordid><startdate>20121201</startdate><enddate>20121201</enddate><creator>Petrovsky, M. N.</creator><creator>Savchenko, E. A.</creator><creator>Kalachev, V. Yu</creator><general>SP MAIK Nauka/Interperiodica</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20121201</creationdate><title>Formation of eudialyte-bearing phonolite from Kontozero carbonatite paleovolcano, Kola Peninsula</title><author>Petrovsky, M. N. ; Savchenko, E. A. ; Kalachev, V. Yu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a311t-824e51f6a2bad7c712f82c9156c913aa20503f34ba7a6ce58fd23f261a2064a73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Mineral Resources</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Petrovsky, M. N.</creatorcontrib><creatorcontrib>Savchenko, E. A.</creatorcontrib><creatorcontrib>Kalachev, V. Yu</creatorcontrib><collection>CrossRef</collection><jtitle>Geology of ore deposits</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Petrovsky, M. N.</au><au>Savchenko, E. A.</au><au>Kalachev, V. Yu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Formation of eudialyte-bearing phonolite from Kontozero carbonatite paleovolcano, Kola Peninsula</atitle><jtitle>Geology of ore deposits</jtitle><stitle>Geol. Ore Deposits</stitle><date>2012-12-01</date><risdate>2012</risdate><volume>54</volume><issue>7</issue><spage>540</spage><epage>556</epage><pages>540-556</pages><issn>1075-7015</issn><eissn>1555-6476</eissn><abstract>The results of the geological and petrologic study of eudialyte-bearing phonolite from the Late Devonian Kontozero carbonatite paleovolcano are discussed in the paper. This eudialyte-bearing phonolite corresponds to the primary melt derived from the metasomatized upper mantle source composed of phlogopite-amphibole eclogite. The average ZrO
2
content in the Kontozero phonolite (1.02 wt %) is considered to be cotectic (Kogarko et al., 1988). Similar REE patterns of the Kontozero eudialyte-bearing phonolite and porphyritic lujavrite from the chilled contact zone of the Lovozero eudyalite complex and close REE and Zr concentrations in the compared rocks show that this complex could have been formed from a melt similar in composition to the phonolite melt of Kontozero.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S1075701512070057</doi><tpages>17</tpages></addata></record> |
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| subjects | Earth and Environmental Science Earth Sciences Mineral Resources |
| title | Formation of eudialyte-bearing phonolite from Kontozero carbonatite paleovolcano, Kola Peninsula |
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