Инд. авторы:	Sorokin A.A., Ostapenko N.S., Ponomarchuk V.A., Travin A.V.
Заглавие:	40Ar/39Ar age of adularia from veins of the Tokur gold deposit, the Mongolian-Okhotsk Orogenic Belt, Russia
Библ. ссылка:	Sorokin A.A., Ostapenko N.S., Ponomarchuk V.A., Travin A.V. 40Ar/39Ar age of adularia from veins of the Tokur gold deposit, the Mongolian-Okhotsk Orogenic Belt, Russia // Geology of Ore Deposits. - 2011. - Vol.53. - Iss. 3. - P.264-271. - ISSN 1075-7015. - EISSN 1555-6476.
Внешние системы:	DOI: 10.1134/S1075701511030081; SCOPUS: 2-s2.0-79960153128;
Реферат:	eng: The 40Ar/39Ar age of the productive stage of the ore-forming hydrothermal process at the large Tokur gold deposit is 122.4 ± 2.0 Ma. This estimate suggests a paragenetic relationship of this deposit with the nearly exposed Karaurak subvolcanic trachyrhyodacite intrusion, the U-Pb zircon age of which was previously estimated at 120 ± 5 Ma. The age of mineralization at the Tokur deposit is close to the time of formation of some other deposits in the Russian Far East localized in various structural units. © 2011 Pleiades Publishing, Ltd.
Ключевые слова:	Ore-forming; Orogenic belts; Russian far east; Structural unit; U-Pb zircon; Deposits; Lead; Silicate minerals; Gold deposits; Russian Federation; Russian Far East; Mongol-Okhotsk Fold Belt; zircon; uranium-lead dating; orogenic belt; ore deposit; mineralization; igneous intrusion; hydrothermal alteration; gold; argon-argon dating; Hydrothermal process; adularia;
Издано:	2011
Физ. характеристика:	с.264-271