Инд. авторы:	Deev E.V., Kokh S.N., Sokol E.V., Zolnikov I.D., Panov V.S.
Заглавие:	Mud volcanism as an indicator of late to neopleistocene-holocene activity of the Chilik-Kemin fault, Yli depression, Northern Tien Shan
Библ. ссылка:	Deev E.V., Kokh S.N., Sokol E.V., Zolnikov I.D., Panov V.S. Mud volcanism as an indicator of late to neopleistocene-holocene activity of the Chilik-Kemin fault, Yli depression, Northern Tien Shan // Doklady Earth Sciences. - 2014. - Vol.459. - Iss. 1. - P.1338-1343. - ISSN 1028-334X. - EISSN 1531-8354.
Внешние системы:	DOI: 10.1134/S1028334X1411018X; РИНЦ: 24011781; SCOPUS: 2-s2.0-84914696738; WoS: 000346005200005;
Реферат:	eng: It is revealed that the Altyn-Emel mud volcanic field (43°52′56″ N, 79°06′31″ E) in the Yli depression (Dzharkent trough) is structurally linked to the northeastern end of the Chilik-Kemin deep fault. The mud volcano is related to hydrocarbon-rich gases (including methane) and pressure artesian mineralized thermal waters, which uplifted to the surface along the fault zone. It is suggested that the earthquakes with M≤ 5 related both to the Chilik-Kemin fault and other seismic generating structures intensified the mud volcanic activity. In some cases, the eruptions were accompanied by the short-lived ignition of hydrocarbon gases and formation of the Na-rich paralavas. The mud volcanism of the Altyn-Emel field has been manifested during the last 15–20 k.a., and, consequently, the northeastern part of the Chilik-Kemin fault is an active structure. © 2014, Pleiades Publishing, Ltd.
Ключевые слова:	volcanism; volcanic eruption; Pleistocene; mud volcano; hydrocarbon; Holocene; fault zone; Volcanoes; Volcanic field; Volcanic activities; Thermal waters; Mud volcanoes; Mud volcanism; Fault zone; Deep fault; Active structures; Methane; Earthquakes; Tien Shan;
Издано:	2014
Физ. характеристика:	с.1338-1343