Инд. авторы: Ripp G.S., Izbrodin I.A., Doroshkevich A.G., Lastochkin E.I., Rampilov M.O., Sergeev S.A., Travin A.V., Posokhov V.F.
Заглавие: Chronology of the formation of the gabbro-syenite-granite series of the Oshurkovo pluton, western Transbaikalia
Библ. ссылка: Ripp G.S., Izbrodin I.A., Doroshkevich A.G., Lastochkin E.I., Rampilov M.O., Sergeev S.A., Travin A.V., Posokhov V.F. Chronology of the formation of the gabbro-syenite-granite series of the Oshurkovo pluton, western Transbaikalia // Petrology. - 2013. - Vol.21. - Iss. 4. - P.375-392. - ISSN 0869-5911. - EISSN 1556-2085.
Внешние системы: DOI: 10.1134/S0869591113030053; SCOPUS: 2-s2.0-84880495043; WoS: 000321787900005;
Реферат: eng: This paper reports the results of Rb-Sr, 40Ar-39Ar, and U-Pb geochronological investigations for igneous and metamorphic rocks from the regions of the Oshurkovo basic massif. It was shown that the gabbro-syenite-granite complex that was formed there is similar to the bimodal basalt-rhyolite series of volcanic associations. Three major stages of magmatic activity were recognized: syenite-granite (132-127 Ma), basic (126-117 Ma), and granite (121-112 Ma). The silicic igneous rocks were formed owing to anatexis under the influence of heat released from the parent chamber of alkaline gabbroids. © 2013 Pleiades Publishing, Ltd.
Издано: 2013
Физ. характеристика: с.375-392