Тип публикации: статья из журнала
Год издания: 2009
Идентификатор DOI: 10.1134/S1028334X09060166
Ключевые слова: Earth's crust, Isotope compositions, Isotope data, Magma sources, Magmatisms, Mantle source, New model, Rare elements, SIBERIA, Volcano-plutonic structure, Strontium, Isotopes, isotopic composition, magmatism, neodymium isotope, pluton, strontium isotope
Аннотация: The first data are presented on the distribution of rare elements and isotope composition of neodymium and strontium in the rocks of the alkaline-ultramafitic association of the Kresty volcanoplutonic structure (one of the probable satellites of the Gulinian massif being the largest in the Maimecha-Kotui alkaline province in Polar Siberia). On the basis of the results of geochemical studies performed and formerly obtained geophysical and isotope data, a new model is proposed for the plume nature of magmatism in the region, based on the action of a single mantle source of the PREMA type and its active interaction with the matter of the Earth's crust.
Издание
Журнал: DOKLADY EARTH SCIENCES
Выпуск журнала: Vol. 427, Is. 2
Номера страниц: 961-967
ISSN журнала: 1028334X
Место издания: NEW YORK
Издатель: MAIK NAUKA/INTERPERIODICA/SPRINGER
Персоны
- Gertner I.F. (Tomsk State University)
- Vrublevskii V.V. (Tomsk State University)
- Krasnova T.S. (Tomsk State University)
- Tishin P.A. (Tomsk State University)
- Voitenko D.N. (Tomsk State University)
- Sazonov A.M. (Siberian Federal University)
- Zvyagina E.A. (Siberian Federal University)
- Kolmakov Y.V. (Tomsk Polytechnic University)
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