著者

溝上 恵

出版者

東京大学地震研究所

雑誌

地震研究所研究速報

巻号頁・発行日

vol.12, pp.41-56, 1974-03

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It should be emphasized that when using an array to determine directly dT/dΔ for the study of the structure of the Earth's deep interior, the necessity for the correction for the near surface structures is inevitable, particularly in such a region as the Kii Peninsula where existence of a dipping Moho-discontinuity is expected. A teleseismic slowness vector analysis method given by Zengeni(1970) is applied for the study of the diwing Moho-discontinuity in the Kii Peninsula.