2024-03-29T11:46:51Z
https://repository.dl.itc.u-tokyo.ac.jp/oai
oai:repository.dl.itc.u-tokyo.ac.jp:00033077
2022-12-19T04:08:46Z
80:4535:4827:4833
9:504:4538:4829:4834
Tectonic Stress and Viscosity Coefficient of the Earth's Crust as inferred from Crustal Movements related with Active Folds
活褶曲から推定される造構応力と地殻の粘性について
溝上, 恵
128995
453
application/pdf
It has been pointed out from geological and geomorphological evidences that the time rate of undulatory crustal movement shows a remarkable dependence on its wavelength. Specific studies on the problem were made by MATSUDA (1960, 1961, 1964), KAIZUKA (1967, 1968) and OTA (1968, 1969). KAIZUKA compared the rate of folding in the Quaternary with the mode of undulatory crustal movements in the present. He indicated such regularities of folding as the smaller the wavelength, the greater the rate of folding and the rate of present folding is in the same order with that of the Quaternary folding.
departmental bulletin paper
東京大学地震研究所
1980-11-15
application/pdf
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo
2
55
483
504
AN00162258
00408972
https://repository.dl.itc.u-tokyo.ac.jp/record/33077/files/ji0552007.pdf
jpn