Zobrazeno 1 - 10
of 96
pro vyhledávání: '"Richard H. Sibson"'
Autor:
Richard H. Sibson
Publikováno v:
Earth, Planets and Space, Vol 72, Iss 1, Pp 1-20 (2020)
Abstract A combination of geological evidence (in the form of hydrothermal vein systems in exhumed fault systems) and geophysical information around active faults supports the localized invasion of near-lithostatically overpressured aqueous fluids in
Externí odkaz:
https://doaj.org/article/aa26d63d74814707af5498d6fa26c37d
Autor:
Yoshihisa Iio, Richard H. Sibson, Toru Takeshita, Takeshi Sagiya, Bunichiro Shibazaki, T. Junichi Nakajima
Publikováno v:
Earth, Planets and Space, Vol 70, Iss 1, Pp 1-4 (2018)
Externí odkaz:
https://doaj.org/article/b6ac1ee9cc2342a89181e9cca23bc1de
Autor:
Richard H. Sibson
Publikováno v:
Earth, Planets and Space, Vol 69, Iss 1, Pp 1-15 (2017)
Abstract Hydrothermal extension veins form by hydraulic fracturing under triaxial stress (principal compressive stresses, σ 1 > σ 2 > σ 3) when the pore-fluid pressure, P f, exceeds the least compressive stress by the rock’s tensile strength. Su
Externí odkaz:
https://doaj.org/article/35c6eccd08004143b19b41cea7725b32
Autor:
Yoshihisa Iio, Richard H. Sibson, Toru Takeshita, Takeshi Sagiya, Bunichiro Shibazaki, Junichi Nakajima
Publikováno v:
Earth, Planets and Space, Vol 71, Iss 1, Pp 1-1 (2019)
In the original publication of this article [1], the co-author’s name “T. Junichi Nakajima” in the author list should be “Junichi Nakajima”.
Externí odkaz:
https://doaj.org/article/87bd554e70e14590a8a683621bbf15af
Autor:
Richard H. Sibson
Publikováno v:
Bulletin of the Seismological Society of America. 110:850-862
Frictional instability leading to fault rupture may be driven by increasing differential stress or by increases in pore-fluid pressure within the rock mass. Geological evidence (from hydrothermal vein systems in exhumed faults) together with geophysi
Autor:
Richard H. Sibson
Publikováno v:
Geoscience Frontiers, Vol 10, Iss 6, Pp 2093-2100 (2019)
In quartzo-feldspathic continental crust with moderate-to-high heat flow, seismic activity extends to depths of 10–20 km, bounded by isotherms in the 350–450 °C range. Fluid overpressuring above hydrostatic in seismogenic crust, is heterogeneous
Autor:
Yoshihisa Iio, Tomomi Okada, Tsutomu Miura, Francesca Ghisetti, Satoshi Matsumoto, Jarg R. Pettinga, Shiro Ohmi, Tadashi Sato, Stephen Bannister, Shintaro Horiuchi, Richard H. Sibson
Publikováno v:
Tectonophysics. 765:172-186
Actively deforming crust and upper mantle around the obliquely convergent Pacific-Australia plate boundary in the northern South Island of New Zealand have been investigated by seismic tomography using data from a temporary c. 50 station network plus
Autor:
Stephen Bannister, Akiko Toh, Satoshi Matsumoto, Satoshi Ide, Tomomi Okada, Calum J. Chamberlain, F. Aden-Antoniow, Ryosuke Ando, Richard H. Sibson, Yoshihisa Iio, Pierre Romanet
Seismic tremor has previously been reported in the Marlborough (New Zealand) region, with detections made using the national GeoNet network. However, because of the sparsity of that network, only 40 tremors were detected using 6 stations. We conducte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2108d6b19adb83819f81c26e54323435
https://doi.org/10.5194/egusphere-egu21-637
https://doi.org/10.5194/egusphere-egu21-637
Autor:
Miu Matsuno, Ayaka Tagami, Tomomi Okada, Satoshi Matsumoto, Yuta Kawamura, Yoshihisa Iio, Tadashi Sato, Takashi Nakayama, Satoshi Hirahara, Stephen Bannister, John Ristau, Martha K. Savage, Clifford H. Thurber, Richard H. Sibson
Publikováno v:
Tectonophysics. 835:229390
Publikováno v:
New Zealand Journal of Geology and Geophysics. 61:461-479
The subsurface structure of the Moutere Depression is obscured by a thick Plio-Quaternary gravel sequence. Surface and subsurface data have been used to define a blind basement pop-up bounded to th...