Инд. авторы:	Buchko I.V., Sorokin A.A., Ponomarchuk A.V., Travin A.V., Ponomarchuk V.A.
Заглавие:	Ar-40/Ar-39 Age of the Porphyry Ca(Au) Mineralization of the Elna Deposit and Its Relation to Magmatism (Northeastern Part of the Argun Superterrane)
Библ. ссылка:	Buchko I.V., Sorokin A.A., Ponomarchuk A.V., Travin A.V., Ponomarchuk V.A. Ar-40/Ar-39 Age of the Porphyry Ca(Au) Mineralization of the Elna Deposit and Its Relation to Magmatism (Northeastern Part of the Argun Superterrane) // Doklady Earth Sciences. - 2017. - Vol.472. - Iss. 1. - P.62-66. - ISSN 1028-334X. - EISSN 1531-8354.
Внешние системы:	DOI: 10.1134/S1028334X17010111; SCOPUS: 2-s2.0-85017628231; WoS: 000399720600014;
Реферат:	eng: The Elna Cu(Au)-porphyry deposit is one of the typical ore objects in the northeastern margin of the Argun superterrane facing the Mongolia-Okhotsk foldbelt. Mineralization includes zones of argillization with fine quartz veins in granodiorite of the Elna massif. The geochronological Ar-40/Ar-39 studies of hydrothermal near-ore metasomatites and magmatic rocks of the deposit show that the age of host granitoids is 126 +/- 2 Ma, which corresponds to the upper age boundary of granitoids from the Burinda Complex, whereas the age of overprinted hydrothermal processes is 122-117 Ma. The age of mineralization correlates well with the age of the thermal event in East Asia. An intense stage of magmatism including both volcanic and intrusive forms occurred in this period.
Ключевые слова:	GRANITOIDS; MARGIN; GEOCHRONOLOGY; WESTERN-PART; METAL DEPOSIT; NORTH-ASIAN CRATON; METALLOGENIC ZONE; REGION;
Издано:	2017
Физ. характеристика:	с.62-66