A New Ectasian Event of Basitic Magmatism in the Southern Siberian Craton
On the basis of U–Pb dating of zircon and baddeleyite from gabbro–dolerite of the Goloustnaya dyke swarm (southern margin of the Siberian Craton), the age of basites was established as 1338.0 ± 2.9 Ma. It is shown that the basite intrusions of close ages from the Goloustnaya and Listvyanka areas (so...
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| Veröffentlicht in: | Doklady earth sciences 2019-05, Vol.486 (1), p.507-511 |
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| container_title | Doklady earth sciences |
| container_volume | 486 |
| creator | Gladkochub, D. P. Donskaya, T. V. Ernst, R. E. Hamilton, M. A. Mazukabzov, A. M. Pisarevsky, S. A. Kamo, S. |
| description | On the basis of U–Pb dating of zircon and baddeleyite from gabbro–dolerite of the Goloustnaya dyke swarm (southern margin of the Siberian Craton), the age of basites was established as 1338.0 ± 2.9 Ma. It is shown that the basite intrusions of close ages from the Goloustnaya and Listvyanka areas (southern Siberian Craton) and Victoria Island (northern Laurentia, Barking Dog complex) could have been formed under the influence of the same mantle plume and belong to the same Large Igneous Province of Ectasian (Middle Mesoproterozoic) age. |
| doi_str_mv | 10.1134/S1028334X19050222 |
| format | Article |
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It is shown that the basite intrusions of close ages from the Goloustnaya and Listvyanka areas (southern Siberian Craton) and Victoria Island (northern Laurentia, Barking Dog complex) could have been formed under the influence of the same mantle plume and belong to the same Large Igneous Province of Ectasian (Middle Mesoproterozoic) age.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X19050222</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Cratons ; Earth ; Earth and Environmental Science ; Earth Sciences ; Gabbro ; Geological time ; Geology ; Magma ; Magmatism ; Mantle ; Mantle plumes ; Radiometric dating ; Rock intrusions ; Zircon</subject><ispartof>Doklady earth sciences, 2019-05, Vol.486 (1), p.507-511</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-a378t-74f4424c44b9a3ea776adef28829100cdc8a7446cfd8d9a6dd4fcebdad2745d83</citedby><cites>FETCH-LOGICAL-a378t-74f4424c44b9a3ea776adef28829100cdc8a7446cfd8d9a6dd4fcebdad2745d83</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/S1028334X19050222$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1028334X19050222$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Gladkochub, D. 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It is shown that the basite intrusions of close ages from the Goloustnaya and Listvyanka areas (southern Siberian Craton) and Victoria Island (northern Laurentia, Barking Dog complex) could have been formed under the influence of the same mantle plume and belong to the same Large Igneous Province of Ectasian (Middle Mesoproterozoic) age.</description><subject>Cratons</subject><subject>Earth</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Gabbro</subject><subject>Geological time</subject><subject>Geology</subject><subject>Magma</subject><subject>Magmatism</subject><subject>Mantle</subject><subject>Mantle plumes</subject><subject>Radiometric dating</subject><subject>Rock intrusions</subject><subject>Zircon</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp1kEtLAzEUhYMoWKs_wF3A9dQ87sxklrVULVRdVMHdkOZRU9pMTVLFf2_KCC5EsjjJvee7uRyELikZUcrhekEJE5zDK21ISRhjR2hAS04LwUs4zvfcLg79U3QW45oQACibAZqN8aP5xFOVZHTS4-mH8Ql3Ft_kd3IKP8jVViYXt9h5nN4MXnT7LMHjhVuacGAmQabOn6MTKzfRXPzoEL3cTp8n98X86W42Gc8LyWuRihosAAMFsGwkN7KuK6mNZUKwhhKitBKyBqiU1UI3stIarDJLLTWrodSCD9FVP3cXuve9ialdd_vg85ctYwA14byps2vUu1ZyY1rnbZeCVPlos3Wq88a6XB-XDaEVEzmpIaI9oEIXYzC23QW3leGrpaQ9RNz-iTgzrGdi9vqVCb-r_A99A6iQfHc</recordid><startdate>20190501</startdate><enddate>20190501</enddate><creator>Gladkochub, D. 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| subjects | Cratons Earth Earth and Environmental Science Earth Sciences Gabbro Geological time Geology Magma Magmatism Mantle Mantle plumes Radiometric dating Rock intrusions Zircon |
| title | A New Ectasian Event of Basitic Magmatism in the Southern Siberian Craton |
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