Seismic structure and origin of active intraplate volcanoes in Northeast Asia

Tectonophysics

Volumn 470, Issue 3-4, 2009, Pages 257-266

  Duan, Yonghong ^a,b   Zhao, Dapeng ^b   Zhang, Xiankang ^a   Xia, Shaohong ^b   Liu, Zhi ^a   Wang, Fuyun ^a   Li, Li ^a  

^a INSTITUTE OF GEOPHYSICS   (China)

^b TOHOKU UNIVERSITY   (Japan)

Author keywords

Changbai volcano; Hunchun deep earthquakes; P wave velocity structure; Stagnant Pacific slab; Teleseismic tomography

Indexed keywords

CHANGBAI VOLCANO; HUNCHUN DEEP EARTHQUAKES; P-WAVE VELOCITY STRUCTURE; STAGNANT PACIFIC SLAB; TELESEISMIC TOMOGRAPHY;

ACOUSTIC WAVE VELOCITY; DEHYDRATION; EARTHQUAKES; MINING; SEISMOGRAPHS; TECTONICS; THREE DIMENSIONAL; TOMOGRAPHY;

VOLCANOES;

ACCRETIONARY PRISM; ARRIVAL TIME; DEHYDRATION; INTRAPLATE PROCESS; MAGMATISM; MANTLE STRUCTURE; P-WAVE; S-WAVE; SEISMIC TOMOGRAPHY; SEISMOLOGY; SUBDUCTION ZONE; TELESEISMIC WAVE; TRANSITION ZONE; VELOCITY STRUCTURE; VOLCANO; WAVE VELOCITY;

ASIA; CHANGBAI MOUNTAINS; EURASIA; FAR EAST; TIANCHI VOLCANO;

EID: 67349132341     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.tecto.2009.01.004     Document Type: Article

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