期刊
SCIENCE
卷 296, 期 5573, 页码 1679-1681出版社
AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.1070378
关键词
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Deep long-period tremors were recognized and located in a nonvolcanic region in southwest Japan. Epicenters of the tremors were distributed along the strike of the subducting Philippine Sea plate over a length of 600 kilometers. The depth of the tremors averaged about 30 kilometers, near the Mohorovic discontinuity. Each tremor tasted for at most a few weeks. The location of the tremors within the subduction zone indicates that the tremors may have been caused by fluid generated by dehydration processes from the slab.
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