Petrography, mineralogy and SIMS U-Pb geochronology of 1.9–1.8 Ga carbonatites and associated alkaline rocks of the Central-Aldan magnesiocarbonatite province (South Yakutia, Russia)
The N-S trending Central-Aldan magnesiocarbonatite province is located in the Aldan-Stanovoy shield (South Yakutia, Russia). Several apatite-dolomitic carbonatite occurrences were studied: Seligdar, Muostalaah, Ust-Chulman and Birikeen. Mineralogical and petrographic investigations indicate intense...
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| Veröffentlicht in: | Mineralogy and petrology 2019-06, Vol.113 (3), p.329-352 |
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| creator | Prokopyev, Ilya R. Doroshkevich, Anna G. Sergeev, Sergey A. Ernst, Richard E. Ponomarev, Jean D. Redina, Anna A. Chebotarev, Dmitry A. Nikolenko, Anna M. Dultsev, Vladislav F. Moroz, Tatyana N. Minakov, Alexey V. |
| description | The N-S trending Central-Aldan magnesiocarbonatite province is located in the Aldan-Stanovoy shield (South Yakutia, Russia). Several apatite-dolomitic carbonatite occurrences were studied: Seligdar, Muostalaah, Ust-Chulman and Birikeen. Mineralogical and petrographic investigations indicate intense hydrothermal-metasomatic alteration and metamorphism, which are reflected in the evolution of the mineral parageneses. The primary minerals are fluorapatite, magnetite, ilmenite, dolomite, K-feldspar, phlogopite and accessory zircon, titanite, baddeleyite and thorite. The hydrothermal-metasomatic minerals are quartz, calcite and siderite aggregates with haematite, monazite-(Ce), xenotime-(Y), rutile-(Nb), barite-(Sr), anhydrite, ancylite-(Ce) and rare sulphide mineral phases. Alkaline rocks associated with the Muostalaah complex, were also studied. The following U-Pb ages have been obtained (Ma): 1930 ± 7 for Muostalaah alkaline basic rocks, 1906 ± 6 for Muostalaah carbonatites, and 1880 ± 13 and 1878 ± 17 for Seligdar and Ust-Chulman carbonatites, respectively. |
| doi_str_mv | 10.1007/s00710-019-00661-3 |
| format | Article |
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Several apatite-dolomitic carbonatite occurrences were studied: Seligdar, Muostalaah, Ust-Chulman and Birikeen. Mineralogical and petrographic investigations indicate intense hydrothermal-metasomatic alteration and metamorphism, which are reflected in the evolution of the mineral parageneses. The primary minerals are fluorapatite, magnetite, ilmenite, dolomite, K-feldspar, phlogopite and accessory zircon, titanite, baddeleyite and thorite. The hydrothermal-metasomatic minerals are quartz, calcite and siderite aggregates with haematite, monazite-(Ce), xenotime-(Y), rutile-(Nb), barite-(Sr), anhydrite, ancylite-(Ce) and rare sulphide mineral phases. Alkaline rocks associated with the Muostalaah complex, were also studied. The following U-Pb ages have been obtained (Ma): 1930 ± 7 for Muostalaah alkaline basic rocks, 1906 ± 6 for Muostalaah carbonatites, and 1880 ± 13 and 1878 ± 17 for Seligdar and Ust-Chulman carbonatites, respectively.</description><identifier>ISSN: 0930-0708</identifier><identifier>EISSN: 1438-1168</identifier><identifier>DOI: 10.1007/s00710-019-00661-3</identifier><language>eng</language><publisher>Vienna: Springer Vienna</publisher><subject>Anhydrite ; Apatite ; Barite ; Calcite ; Dolomite ; Dolostone ; Earth and Environmental Science ; Earth Sciences ; Feldspars ; Fluorapatite ; Geochemistry ; Geochronology ; Geochronometry ; Haematite ; Hematite ; Ilmenite ; Inorganic Chemistry ; Isotopes ; Lead ; Magnetite ; Metamorphism ; Metamorphism (geology) ; Mineralogy ; Minerals ; Monazite ; Original Paper ; Petrography ; Petrology ; Radiometric dating ; Rock ; Rocks ; Rutile ; Siderite ; Sulfides ; Sulphide minerals ; Sulphides ; Thorite ; Titanite ; Xenotime ; Zircon</subject><ispartof>Mineralogy and petrology, 2019-06, Vol.113 (3), p.329-352</ispartof><rights>Springer-Verlag GmbH Austria, part of Springer Nature 2019</rights><rights>Mineralogy and Petrology is a copyright of Springer, (2019). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2343-d072c72fb1da7846e0ca6765060061059f0a249834e62ee1ac858770306f24c43</citedby><cites>FETCH-LOGICAL-c2343-d072c72fb1da7846e0ca6765060061059f0a249834e62ee1ac858770306f24c43</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00710-019-00661-3$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00710-019-00661-3$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Prokopyev, Ilya R.</creatorcontrib><creatorcontrib>Doroshkevich, Anna G.</creatorcontrib><creatorcontrib>Sergeev, Sergey A.</creatorcontrib><creatorcontrib>Ernst, Richard E.</creatorcontrib><creatorcontrib>Ponomarev, Jean D.</creatorcontrib><creatorcontrib>Redina, Anna A.</creatorcontrib><creatorcontrib>Chebotarev, Dmitry A.</creatorcontrib><creatorcontrib>Nikolenko, Anna M.</creatorcontrib><creatorcontrib>Dultsev, Vladislav F.</creatorcontrib><creatorcontrib>Moroz, Tatyana N.</creatorcontrib><creatorcontrib>Minakov, Alexey V.</creatorcontrib><title>Petrography, mineralogy and SIMS U-Pb geochronology of 1.9–1.8 Ga carbonatites and associated alkaline rocks of the Central-Aldan magnesiocarbonatite province (South Yakutia, Russia)</title><title>Mineralogy and petrology</title><addtitle>Miner Petrol</addtitle><description>The N-S trending Central-Aldan magnesiocarbonatite province is located in the Aldan-Stanovoy shield (South Yakutia, Russia). Several apatite-dolomitic carbonatite occurrences were studied: Seligdar, Muostalaah, Ust-Chulman and Birikeen. Mineralogical and petrographic investigations indicate intense hydrothermal-metasomatic alteration and metamorphism, which are reflected in the evolution of the mineral parageneses. The primary minerals are fluorapatite, magnetite, ilmenite, dolomite, K-feldspar, phlogopite and accessory zircon, titanite, baddeleyite and thorite. The hydrothermal-metasomatic minerals are quartz, calcite and siderite aggregates with haematite, monazite-(Ce), xenotime-(Y), rutile-(Nb), barite-(Sr), anhydrite, ancylite-(Ce) and rare sulphide mineral phases. Alkaline rocks associated with the Muostalaah complex, were also studied. The following U-Pb ages have been obtained (Ma): 1930 ± 7 for Muostalaah alkaline basic rocks, 1906 ± 6 for Muostalaah carbonatites, and 1880 ± 13 and 1878 ± 17 for Seligdar and Ust-Chulman carbonatites, respectively.</description><subject>Anhydrite</subject><subject>Apatite</subject><subject>Barite</subject><subject>Calcite</subject><subject>Dolomite</subject><subject>Dolostone</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Feldspars</subject><subject>Fluorapatite</subject><subject>Geochemistry</subject><subject>Geochronology</subject><subject>Geochronometry</subject><subject>Haematite</subject><subject>Hematite</subject><subject>Ilmenite</subject><subject>Inorganic Chemistry</subject><subject>Isotopes</subject><subject>Lead</subject><subject>Magnetite</subject><subject>Metamorphism</subject><subject>Metamorphism (geology)</subject><subject>Mineralogy</subject><subject>Minerals</subject><subject>Monazite</subject><subject>Original 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minerals</subject><subject>Sulphides</subject><subject>Thorite</subject><subject>Titanite</subject><subject>Xenotime</subject><subject>Zircon</subject><issn>0930-0708</issn><issn>1438-1168</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp9kcFuEzEQhi0EEqHwApwscQGpDmN74_Ueq6i0lYqoCD1wsiaOd7PNxg62Fyk33oEX6Gtw5VF4EtwECU5cPJbm_78ZzU_ISw5TDlC_TeXhwIA3DEApzuQjMuGV1IxzpR-TCTSytGvQT8mzlO4AQM80n5AfNy7H0EXcrfendNt7F3EI3Z6iX9HF1fsFvWU3S9q5YNcx-HDohZbyafPr23c-1T_vL5BajMvgMffZpYMTUwq2x-zKd9jgULg0BrtJD968dnTufC6T2NmwQk-32HmX-vAPh-5i-Np76-jrRRjzmn7GzZh7PKUfx5R6fPOcPGlxSO7Fn3pCbt-df5pfsusPF1fzs2tmhawkW0EtbC3aJV9hrSvlwKKq1QxUORSHWdMCiqrRsnJKOMfRlsPUNUhQrahsJU_IqyO3LPRldCmbuzBGX0YaIUBpUWC6qMRRZWNIKbrW7GK_xbg3HMxDROYYkSkRmUNERhaTPJpSEfvOxb_o_7h-AyE8li4</recordid><startdate>20190601</startdate><enddate>20190601</enddate><creator>Prokopyev, 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Petrol</stitle><date>2019-06-01</date><risdate>2019</risdate><volume>113</volume><issue>3</issue><spage>329</spage><epage>352</epage><pages>329-352</pages><issn>0930-0708</issn><eissn>1438-1168</eissn><abstract>The N-S trending Central-Aldan magnesiocarbonatite province is located in the Aldan-Stanovoy shield (South Yakutia, Russia). Several apatite-dolomitic carbonatite occurrences were studied: Seligdar, Muostalaah, Ust-Chulman and Birikeen. Mineralogical and petrographic investigations indicate intense hydrothermal-metasomatic alteration and metamorphism, which are reflected in the evolution of the mineral parageneses. The primary minerals are fluorapatite, magnetite, ilmenite, dolomite, K-feldspar, phlogopite and accessory zircon, titanite, baddeleyite and thorite. The hydrothermal-metasomatic minerals are quartz, calcite and siderite aggregates with haematite, monazite-(Ce), xenotime-(Y), rutile-(Nb), barite-(Sr), anhydrite, ancylite-(Ce) and rare sulphide mineral phases. Alkaline rocks associated with the Muostalaah complex, were also studied. The following U-Pb ages have been obtained (Ma): 1930 ± 7 for Muostalaah alkaline basic rocks, 1906 ± 6 for Muostalaah carbonatites, and 1880 ± 13 and 1878 ± 17 for Seligdar and Ust-Chulman carbonatites, respectively.</abstract><cop>Vienna</cop><pub>Springer Vienna</pub><doi>10.1007/s00710-019-00661-3</doi><tpages>24</tpages></addata></record> |
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| subjects | Anhydrite Apatite Barite Calcite Dolomite Dolostone Earth and Environmental Science Earth Sciences Feldspars Fluorapatite Geochemistry Geochronology Geochronometry Haematite Hematite Ilmenite Inorganic Chemistry Isotopes Lead Magnetite Metamorphism Metamorphism (geology) Mineralogy Minerals Monazite Original Paper Petrography Petrology Radiometric dating Rock Rocks Rutile Siderite Sulfides Sulphide minerals Sulphides Thorite Titanite Xenotime Zircon |
| title | Petrography, mineralogy and SIMS U-Pb geochronology of 1.9–1.8 Ga carbonatites and associated alkaline rocks of the Central-Aldan magnesiocarbonatite province (South Yakutia, Russia) |
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