Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Mitsuhiko Shimada"'
Publikováno v:
Tectonophysics. 323:61-76
We investigated the gross structure of a fault in three dimensions during its formation process. The observed sample was Westerly granite recovered from compression after peak stress but before dynamic rupture. The sample was infused with a fluoresce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ffd977f497df02ce6c9166d95b0427f
https://doi.org/10.1016/s0040-1951(00)00088-3
https://doi.org/10.1016/s0040-1951(00)00088-3
Publikováno v:
Tectonophysics. 313:293-305
Observations of spatial fault development in granite undergoing compression provide new insights into the process of faulting. Dry intact Westerly granite samples were loaded under a confining pressure of 100 MPa (triaxial conditions) and 5 MPa (∼
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d25b7d50a4e1dfd2236430c83d67ded
https://doi.org/10.1016/s0040-1951(99)00205-x
https://doi.org/10.1016/s0040-1951(99)00205-x
Autor:
Mitsuhiko Shimada
Publikováno v:
Zisin (Journal of the Seismological Society of Japan. 2nd ser.). 48:177-185
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c76961714511a322b06003c777e0d4aa
https://doi.org/10.4294/zisin1948.48.1_177
https://doi.org/10.4294/zisin1948.48.1_177
Autor:
Mitsuhiko Shimada
Publikováno v:
Tectonophysics. 217:55-64
A model is proposed for the strength of the crust or lithosphere, in which the peak strength is in the brittle regime, but not on the brittle-ductile transition. The model is based on experimental evidence which suggests that the fracture mechanism c
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https://explore.openaire.eu/search/publication?articleId=doi_________::769fdd6b0075db995301b4441ba40b4c
https://doi.org/10.1016/0040-1951(93)90202-u
https://doi.org/10.1016/0040-1951(93)90202-u
Autor:
Mitsuhiko Shimada
Publikováno v:
THE REVIEW OF HIGH PRESSURE SCIENCE AND TECHNOLOGY. 2:151-160
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e16aecb79405f2c7b72978c84b6c6b0
https://doi.org/10.4131/jshpreview.2.151
https://doi.org/10.4131/jshpreview.2.151
Autor:
Mitsuhiko Shimada
Publikováno v:
Tectonophysics. 211:259-268
Shimada, M., 1992. Confirmation of two types of fracture in granite deformed at temperatures to 300°C. In: T. Mikumo, K. Aki, M. Ohnaka, L.J. Ruff and P.K.P. Spudich (Editors), Earthquake Source Physics and Earthquake Precursors. Tectonophysics, 211
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5ed09a9bc60a9b91b54f1e7523204fcc
https://doi.org/10.1016/0040-1951(92)90063-c
https://doi.org/10.1016/0040-1951(92)90063-c
Autor:
Akio Cho, Mitsuhiko Shimada
Publikováno v:
Tectonophysics. 175:221-235
Four silicate rocks (granite, gabbro, dunite and eclogite) were triaxially compressed up to a confining pressure of 3 GPa at room temperature and were found to exhibit brittle fracture behaviour. From the measurements of the compressive and frictiona
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2edba02dfc8e274ca7d831e5612ef55e
https://doi.org/10.1016/0040-1951(90)90139-y
https://doi.org/10.1016/0040-1951(90)90139-y
Autor:
Mitsuhiko Shimada
Publikováno v:
THE REVIEW OF HIGH PRESSURE SCIENCE AND TECHNOLOGY. 5:122-123
The full knowledge of the state of stress in the earth' s crust is indispensable for earthquake prediction research. Today, the crustal stress is measured only intermittently at limited sites by several methods, but not continuously. There are some d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e44267d5079d6e99e2ad84b03b97a9b6
https://doi.org/10.4131/jshpreview.5.122
https://doi.org/10.4131/jshpreview.5.122
Publikováno v:
International Journal of Rock Mechanics and Mining Sciences. 34:151.e1-151.e12
Observations of the spatial development of cracks in granite undergoing triaxial compression provide new insights into the proces of fault formation. Dry intact Westerly granite samples were loaded under confining pressure of 100 MPa, and the progres
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a27f87536b2086778f999ebcc1385e7
https://doi.org/10.1016/s1365-1609(97)00138-x
https://doi.org/10.1016/s1365-1609(97)00138-x
Autor:
Mitsuhiko Shimada
Publikováno v:
Journal of Geophysical Research. 96:11877
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::427e282a1bf937edffd7661f29256baa
https://doi.org/10.1029/91jb01075
https://doi.org/10.1029/91jb01075