Temporal change of characteristics of shallow volcano-tectonic earthquakes associated with increase in volcanic activity at Kuchinoerabujima volcano, Japan

Journal of Volcanology and Geothermal Research

Volumn 187, Issue 1-2, 2009, Pages 1-12

  Triastuty, Hetty ^a,b   Iguchi, Masato ^b   Tameguri, Takeshi ^b  

^a Center for Volcanology and Geological Hazard Mitigation   (Indonesia)

^b KYOTO UNIVERSITY   (Japan)

Author keywords

corner frequency; fracture zone; Kuchinoerabujima volcano; shallow VT earthquake

Indexed keywords

CORNER FREQUENCY; FLUID-FILLED; FOCAL MECHANISM; FRACTURE ZONE; FRACTURED ZONES; HYDROTHERMAL ACTIVITY; HYDROTHERMAL FLUIDS; ISLAND VOLCANO; KUCHINOERABUJIMA VOLCANO; LOW FREQUENCY; NORMAL FAULTS; PRESSURE FIELD; PRESSURE INCREASE; RUPTURE LENGTH; SHALLOW VT EARTHQUAKE; STRESS FIELD; TEMPORAL CHANGE; VOLCANIC ACTIVITIES; VOLCANIC SYSTEMS; VOLCANO TECTONIC EARTHQUAKES;

CRACKS; EARTHQUAKES; ENGINEERING GEOLOGY; FRACTURE; MONOCHROMATORS; TECTONICS;

VOLCANOES;

EARTHQUAKE HYPOCENTER; EARTHQUAKE RUPTURE; FOCAL MECHANISM; FRACTURE ZONE; HYDROTHERMAL ACTIVITY; HYDROTHERMAL FLUID; NORMAL FAULT; SEISMICITY; STRESS FIELD; TECTONICS; VOLCANIC EARTHQUAKE; VOLCANO;

ASIA; EURASIA; FAR EAST; JAPAN; KAGOSHIMA [KYUSHU]; KUCHINOERABU ISLAND; KYUSHU; OSUMI ISLANDS;

EID: 70349775495     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2009.05.017     Document Type: Article

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