机译:泥火山作用是北天山Yli凹陷Chilik-Kemin断层晚新世新世-全新世活动的指示
Trofimuk Institute for Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090 Russia;
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090 Russia;
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090 Russia;
Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090 Russia;
Institute of Archeology and Ethnography, Siberian Branch, Russian Academy of Sciences, pr. Akademika Lavrent'eva 17, Novosibirsk, 630090 Russia;
机译:Dzhungarian断层:北天山地区晚第四纪构造和主要右侧走滑断层的滑移率
机译:天山北部伊犁盆地逆冲断层和走滑断层缩短
机译:天山北部活动断层:地震危险的构造物理分区
机译:哈萨克斯坦永久性站点从天山北部获得的GPS速度场
机译:中国构造研究:南中国海北缘的伸展构造;天山的融合与隆升;和阿尔金塔格断层的楔形挤压模型。
机译:QTP和天山地区北缘特有的Diptychus maculatus(Cyprinidae)的系统志
机译:Dzhungarian断层:北天山地区晚第四纪构造和主要右侧走滑断层的滑移率