Zobrazeno 1 - 10
of 37
pro vyhledávání: '"Daisuke, Asahina"'
Publikováno v:
Earth, Planets and Space, Vol 74, Iss 1, Pp 1-13 (2022)
Abstract The mineral veins formed by filling tensile cracks record the accumulation of past hydraulic activities such as fluid migration in the damage zones of a fault. The purpose of this study is to estimate the fluid flow behavior around thrust fa
Externí odkaz:
https://doaj.org/article/ce752d9e1fd245bd9e26e395bd1867ba
Publikováno v:
Remote Sensing, Vol 15, Iss 21, p 5177 (2023)
The Wispy Terrain is the region of chasmata characterized by quasi-parallel fault systems, formed by extensional and shear stresses of the icy crust of Dione, a moon of Saturn. Besides the basic, satellite-scale geological mapping and very general de
Externí odkaz:
https://doaj.org/article/01f573304b4645ba989aa79eebfa0980
Publikováno v:
Progress in Earth and Planetary Science, Vol 7, Iss 1, Pp 1-12 (2020)
Abstract Through two lab-scale experiments, we investigated the hydraulic and mechanical characteristics of sediment layers during water film formation, induced by elevated pore pressure—considered one of the triggers of submarine landslides. These
Externí odkaz:
https://doaj.org/article/04154cfce6ca4a8797b61e302653154f
Publikováno v:
Journal of Rock Mechanics and Geotechnical Engineering, Vol 10, Iss 6, Pp 1102-1111 (2018)
In this context, recent developments in the coupled three-dimensional (3D) hydro-mechanical (HM) simulation tool TOUGH-RBSN are presented. This tool is used to model hydraulic fracture in geological media, as observed in laboratory-scale tests. The T
Externí odkaz:
https://doaj.org/article/ccc3f168ee8d4d3aaa087db9cca8cc6f
Publikováno v:
Rock Mechanics and Rock Engineering.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da65a6c134c4453561ddce7fa6119f50
https://doi.org/10.1007/s00603-023-03391-3
https://doi.org/10.1007/s00603-023-03391-3
Publikováno v:
Rock Mechanics and Rock Engineering. 54:4825-4849
En-echelon fractures widely exist in natural rock masses. Although the formation and occurrence features of en-echelon fractures have been extensively studied by geologists, the anisotropic mechanical behavior caused by en-echelon fractures has recei
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::769b6a4283b6f94168d5817dfafcaf83
https://doi.org/10.1007/s00603-021-02555-3
https://doi.org/10.1007/s00603-021-02555-3
Publikováno v:
Rock Mechanics and Engineering Geology in Volcanic Fields ISBN: 9781003293590
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07558faf206827b4092c3cf8fbcf6651
https://doi.org/10.1201/9781003293590-31
https://doi.org/10.1201/9781003293590-31
Publikováno v:
Progress in Earth and Planetary Science, Vol 7, Iss 1, Pp 1-12 (2020)
Through two lab-scale experiments, we investigated the hydraulic and mechanical characteristics of sediment layers during water film formation, induced by elevated pore pressure—considered one of the triggers of submarine landslides. These involved
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::63f11a925c5d99f21303489ba3266bba
http://link.springer.com/article/10.1186/s40645-020-00375-7
http://link.springer.com/article/10.1186/s40645-020-00375-7
Publikováno v:
Rock Mechanics and Rock Engineering. 53:4717-4744
The instability of rock slopes and underground engineering structures is usually caused by shear sliding along discontinuities, such as joints or faults, which are usually non-persistent. It is important to study the shear failure behavior of non-per
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::544d46442755158ad950b44eafea40a8
https://doi.org/10.1007/s00603-020-02186-0
https://doi.org/10.1007/s00603-020-02186-0