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PALEOSEISMIC RUPTURES IN THE POTENTIAL SEISMIC
SOURCE OF THE MAJOR EARTHQUAKES
IN THE DZHUNGAR TIEN SHAN
1 Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia
2 Institute of Disaster Prevention Science and Technology, Beijing, China
3 Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
4 Institute of Earthquake Science, Chinese Earthquake Administration, Beijing, China
2 Institute of Disaster Prevention Science and Technology, Beijing, China
3 Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
4 Institute of Earthquake Science, Chinese Earthquake Administration, Beijing, China
Journal: Problems of Engineering Seismology
Tome: 41
Number: 1
Year: 2014
Pages: 5-18
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ROGOZHIN E..., JUN S., QIFU C., XUHUI S. PALEOSEISMIC RUPTURES IN THE POTENTIAL SEISMIC
SOURCE OF THE MAJOR EARTHQUAKES
IN THE DZHUNGAR TIEN SHAN // . 2014. Т. 41. № 1. С. 5-18.
@article{ROGOZHINPALEOSEISMIC2014,
author = "ROGOZHIN, E. . . and JUN, S. and QIFU, C. and XUHUI, S.",
title = "PALEOSEISMIC RUPTURES IN THE POTENTIAL SEISMIC
SOURCE OF THE MAJOR EARTHQUAKES
IN THE DZHUNGAR TIEN SHAN",
journal = "Problems of Engineering Seismology",
year = 2014,
volume = "41",
number = "1",
pages = "5-18",
doi = "",
language = "English"
}
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Keywords: earthquake, seismic source, fault, escarp, scarp, land-slide, paleosoil, radiocarbon age, anticline, magnitude
Аnnotation: PALEOSEISMIC RUPTURES IN THE POTENTIAL SEISMIC
SOURCE OF THE MAJOR EARTHQUAKES
IN THE DZHUNGAR TIEN SHAN
