Open AccessMapping active magma chambers by b values beneath the off‐Ito volcano, Japan
Author(s) -
Wyss Max,
Shimazaki Kunihiko,
Wiemer Stefan
Publication year - 1997
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/97jb01074
Subject(s) - geology , magma chamber , seismology , magma , volcano , crust , anomaly (physics) , radius , intrusion , magnitude (astronomy) , geophysics , geochemistry , physics , computer security , condensed matter physics , astronomy , computer science
The b value of the frequency‐magnitude relation, and thus the mean magnitude, in the off‐Ito volcanic area is not uniform based on detailed b value tomography using about 10,000 events in an area of 10 km radius and in the upper 15 km of the crust. A high b value anomaly (b=15) below 7 km depth and with a radius of about 2 km, located below the coast southeast of Ito, contrasts with lower values of typically b =0.7 north of it and at shallower depths. On the basis of surface deformations, a tensile crack dislocation source was located above 7 km depth. Thus we surmise that the magma chamber in the off‐Ito area was located below 7 km depth. The correlation of a high b value anomaly with this model supports our hypothesis that active magma chambers may be mapped by high b value anomalies. The magma body may be described as consisting of two parts: a lower, well‐established chamber below 11 km depth and a shallower part (11–7 km depth). The b value in the volume surrounding the magma chamber increased from 0.7 during the 1980s to 1.5 during the earthquake swarms of the 1990s. This may reflect a trend of increasing crack density due to the intrusion activity.