Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Robert L. Kranz"'
Publikováno v:
GEOPHYSICS. 68:690-704
Nonhydrostatic stress, an often‐ignored source of seismic anisotropy, is universally present in the subsurface and may be as common as intrinsic or fracture‐induced anisotropy. Nonhydrostatic stress, applied to an initially transversely isotropic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::09aa7ab8856d460543df40358b3b6e71
https://doi.org/10.1190/1.1567240
https://doi.org/10.1190/1.1567240
Publikováno v:
Mechanical Behavior of Crustal Rocks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d5f8a66cdd0a962d2f8b466da794ab9
https://doi.org/10.1029/gm024p0061
https://doi.org/10.1029/gm024p0061
Publikováno v:
Environmental & Engineering Geoscience. :327-339
Fracture toughness (K [Ic] ) is a measure of the ease with which a fracture can propagate through a rock. The ability to predict fracture toughness from thin sections would allow: a) evaluation of those petrographic characteristics most affecting a r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::650ddfac919b29b9d6d1ecac66099d0d
https://doi.org/10.2113/gseegeosci.xxvii.3.327
https://doi.org/10.2113/gseegeosci.xxvii.3.327
Autor:
Robert L. Kranz
Publikováno v:
Journal of Geophysical Research. 99:15645
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1e3291d2ddeacb7c66fd9db8d68c1754
https://doi.org/10.1029/94jb00493
https://doi.org/10.1029/94jb00493
Autor:
Manabu Takahashi, Osamu Nishizawa, Kinichiro Kusunose, Koji Masuda, Robert L. Kranz, A. Hirata
Publikováno v:
Journal of Geophysical Research: Solid Earth. 96:6171-6171
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::92c5e4d5ae2d6d2636d7d6e06df19301
https://doi.org/10.1029/91jb00114
https://doi.org/10.1029/91jb00114
Autor:
Osamu Nishizawa, Kinichiro Kusunose, Takashi Satoh, Manabu Takahashi, A. Hirata, Robert L. Kranz, Koji Masuda
Publikováno v:
Journal of Geophysical Research. 95:21593
In many geological situations, there is a need to monitor fluid migration and associated phenomena. Acoustic emissions (AE) that result from fluid pressure diffusion from a borehole can potentially provide useful information about migration paths, lo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36204603e59a80515c06b1076068cb6c
https://doi.org/10.1029/jb095ib13p21593
https://doi.org/10.1029/jb095ib13p21593
Autor:
Osamu Nishizawa, Koji Masuda, Robert L. Kranz, Manabu Takahashi, Kinichiro Kusunose, Takashi Satoh
Publikováno v:
Journal of Geophysical Research. 95:21583
During forced water infiltration into a dry granite rock in the dilatant state, migration of a water front and a clear positive feedback between acoustic activity and water flow into microcracks were revealed by means of AE hypocenter locations and v
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c72ea1d6ed7364c3140903570ca9065
https://doi.org/10.1029/jb095ib13p21583
https://doi.org/10.1029/jb095ib13p21583
Publikováno v:
Geophysical Research Letters. 13:1430-1433
Cores from two natural joints were studied to estimate the degree of correlation between the surfaces and the distribution of apertures. Matched pairs of profiles were taken from both surfaces of each joint. These profiles were then placed together t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::448c7bf7b84d236526d43257e7b8420a
https://doi.org/10.1029/gl013i013p01430
https://doi.org/10.1029/gl013i013p01430
Autor:
Robert L. Kranz
Publikováno v:
Tectonophysics. 100:449-480
In the past decade the number of studies about microcracks in rocks has rapidly increased. This review of recent work concentrates on microcracks in rock as separate entities, emphasizing microcrack morphogenesis, kinematics, dynamics, population sta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c28e2c2a829be3e50117071f989083bf
https://doi.org/10.1016/0040-1951(83)90198-1
https://doi.org/10.1016/0040-1951(83)90198-1
Autor:
Robert L. Kranz, James D. Blacic
Publikováno v:
Geophysical Research Letters. 11:975-978
Permeability was measured during creep deformation of a tight sandstone and a granite at upper crustal conditions. With water at 100°C as the pore fluid, permeability first decreased then increased during loading to peak stress. Thereafter, permeabi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62ec7d6802c535e390d0fd7a46fb3010
https://doi.org/10.1029/gl011i010p00975
https://doi.org/10.1029/gl011i010p00975