Isotopic age and heterogeneous sources of gabbro‒anorthosites from the Patchemvarek massif, Kola Peninsula
- Авторлар: Vrevsky A.B.1,2, Lvov A.P.1,2
-
Мекемелер:
- Institute of Precambrian Geology and Geochronology (IGGD RAN)
- St. Petersburg State University
- Шығарылым: Том 469, № 1 (2016)
- Беттер: 716-721
- Бөлім: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/188627
- DOI: https://doi.org/10.1134/S1028334X16070163
- ID: 188627
Дәйексөз келтіру
Аннотация
New U‒Pb (SHRIMP II) data on the age (2661.8 ± 7.1 Ma) and isotopic (Sm‒Nd) composition of the Patchemvarek gabbro‒anorthosite massif located in the junction zone between the Neoarchean Kolmozero-Voron’ya greenstone belt and Keivy paragneiss structure are discussed. The established age and geological‒tectonic position of gabbro‒anorthosites allow the prognostic metallogenic estimate of Ti‒V‒Fe mineralization to be extended to the entire Kolmozero-Voron’ya‒Keivy infrastructural zone of the Kola‒Norwegian province of the Fennoscandian shield.
Авторлар туралы
A. Vrevsky
Institute of Precambrian Geology and Geochronology (IGGD RAN); St. Petersburg State University
Хат алмасуға жауапты Автор.
Email: a.b.vrevsky@ipgg.ru
Ресей, nab. Makarova 2, St. Petersburg, 199034; Universitetskaya nab. 7/9, St. Petersburg, 199106
A. Lvov
Institute of Precambrian Geology and Geochronology (IGGD RAN); St. Petersburg State University
Email: a.b.vrevsky@ipgg.ru
Ресей, nab. Makarova 2, St. Petersburg, 199034; Universitetskaya nab. 7/9, St. Petersburg, 199106
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