REGIONALITY OF CRUST AND UPPER MANTLE STRUCTURE AROUND JAPAN AS DERIVED FROM LARGE EXPLOSIONS AT SEA
RESEARCH Earthquake
GROUP FOR EXPLOSION Research
Institute,
University
SEISMOLOGY of Tokyo
l-l-l
Yayoi,
Bunkyo-ku,
Tokyo
(Japan) (Received
July 18, 1978)
ABSTRACT
Two large explosions (54on) in the Sea of Japan were carried out in July 1976 to study the crust and upper mantle structure around Japan. Seismic waves generated by these explosions were observed at about 50 temporary as well as about 60 permanent stations in Japan up to a distance of about 800 km. Analysis of these data based on the previous information gives the following: (1) The low P,-velocity, 7.5 km/s, beneath northeastern Honshu and the normal P,-velocity beneath the Sea of Japan, 8.1 km/s, were ascertained. (2) In four profiles the crust and upper mantle structure was derived by taking previous results and gravity data into account. (3) There is a possibility that anisotropy of P,-velocity is present beneath Honshu on the Sea of Japan side.