On the age of white anorthosite of the Novomirgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield)
Xenolites of white anorthosites have been found in anorthosites of the main phase of the Novom-irgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield, the Ingul megablock). The age of white anorthosite has been determined by classical uranium-lead method by zircon. Isotopic study of...
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| Дата: | 2014 |
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| Ключові слова: | keywords |
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| Формат: | Стаття |
| Мова: | Російська |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2014
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| Онлайн доступ: | https://journals.uran.ua/geofizicheskiy/article/view/116130 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
Репозитарії
Geofizicheskiy Zhurnal| _version_ | 1866301572357554176 |
|---|---|
| author | Shestopalova, E. E. Stepanyuk, L.M. Dovbush, T. I. Kovtun, A. V. |
| author_facet | Shestopalova, E. E. Stepanyuk, L.M. Dovbush, T. I. Kovtun, A. V. |
| author_sort | Shestopalova, E. E. |
| baseUrl_str | https://journals.uran.ua/geofizicheskiy/oai |
| collection | OJS |
| datestamp_date | 2020-10-07T11:58:11Z |
| description | Xenolites of white anorthosites have been found in anorthosites of the main phase of the Novom-irgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield, the Ingul megablock). The age of white anorthosite has been determined by classical uranium-lead method by zircon. Isotopic study of zircon showed considerable dispersion of values that is possibly caused by heterogeneous internal structure zircon crystals and different combination of generations of different ages. The most ancient, practically concordant age has been obtained for two fractions of light rosy zircon (1796-1806 b. y). that is considerably older than the age of zircon from enclosing anorthosites (1750,2 b. y.) and in our opinion characterizes the age of anorthosite. There are several assumptions as to the origin of xenolites of white anorthosites. They can be the earlier phase of basic rocks of the pluton; a fragment of substance of the lower crust transported from the depth and changed by superposed metasomatic and hydrothermal processes, leucocrate variety of «ancient» anorthosite of AMCHG association, represented by white bronsite anorthosites in the Korosten pluton. |
| doi_str_mv | 10.24028/gzh.0203-3100.v36i2.2014.116130 |
| first_indexed | 2025-07-17T11:06:28Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-116130 |
| institution | Geofizicheskiy Zhurnal |
| keywords_txt_mv | keywords |
| language | Russian |
| last_indexed | 2025-07-17T11:06:28Z |
| publishDate | 2014 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1161302020-10-07T11:58:11Z On the age of white anorthosite of the Novomirgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield) Shestopalova, E. E. Stepanyuk, L.M. Dovbush, T. I. Kovtun, A. V. anorthosite xenolith zircon isotopic dating uranium-lead geochronology method Xenolites of white anorthosites have been found in anorthosites of the main phase of the Novom-irgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield, the Ingul megablock). The age of white anorthosite has been determined by classical uranium-lead method by zircon. Isotopic study of zircon showed considerable dispersion of values that is possibly caused by heterogeneous internal structure zircon crystals and different combination of generations of different ages. The most ancient, practically concordant age has been obtained for two fractions of light rosy zircon (1796-1806 b. y). that is considerably older than the age of zircon from enclosing anorthosites (1750,2 b. y.) and in our opinion characterizes the age of anorthosite. There are several assumptions as to the origin of xenolites of white anorthosites. They can be the earlier phase of basic rocks of the pluton; a fragment of substance of the lower crust transported from the depth and changed by superposed metasomatic and hydrothermal processes, leucocrate variety of «ancient» anorthosite of AMCHG association, represented by white bronsite anorthosites in the Korosten pluton. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-04-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116130 10.24028/gzh.0203-3100.v36i2.2014.116130 Geofizicheskiy Zhurnal; Vol. 36 No. 2 (2014); 150-160 Геофизический журнал; Том 36 № 2 (2014); 150-160 Геофізичний журнал; Том 36 № 2 (2014); 150-160 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116130/110217 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | anorthosite xenolith zircon isotopic dating uranium-lead geochronology method Shestopalova, E. E. Stepanyuk, L.M. Dovbush, T. I. Kovtun, A. V. On the age of white anorthosite of the Novomirgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield) |
| title | On the age of white anorthosite of the Novomirgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield) |
| title_full | On the age of white anorthosite of the Novomirgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield) |
| title_fullStr | On the age of white anorthosite of the Novomirgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield) |
| title_full_unstemmed | On the age of white anorthosite of the Novomirgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield) |
| title_short | On the age of white anorthosite of the Novomirgorod massif of the Korsun-Novomirgorod pluton (the Ukrainian Shield) |
| title_sort | on the age of white anorthosite of the novomirgorod massif of the korsun-novomirgorod pluton (the ukrainian shield) |
| topic | anorthosite xenolith zircon isotopic dating uranium-lead geochronology method |
| topic_facet | anorthosite xenolith zircon isotopic dating uranium-lead geochronology method |
| url | https://journals.uran.ua/geofizicheskiy/article/view/116130 |
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