Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Virginia G. Toy"'
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
In natural friction melts, or pseudotachylites, clast textures and glass compositions can influence the frictional behavior of faults hosting pseudotachylites, and are, in turn, sensitive to the processes involved in pseudotachylite formation. Quanti
Externí odkaz:
https://doaj.org/article/413a68c8964f40b28c85bc23d588d42d
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Open fractures can affect petrophysical properties of their host rock masses, as well as fluid transport and storage, so characterization of them is important to both industrial and research scientists. X-ray Computed Tomography (CT), a non-destructi
Externí odkaz:
https://doaj.org/article/0fb6c7a25df04219a98c31f77d246456
Autor:
Cécile Massiot, Bernard Célérier, Mai‐Linh Doan, Tim A. Little, John Townend, David D. McNamara, Jack Williams, Douglas R. Schmitt, Virginia G. Toy, Rupert Sutherland, Lucie Janku‐Capova, Phaedra Upton, Philippe A. Pezard
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 19, Iss 8, Pp 2492-2515 (2018)
Abstract Ultrasonic image logs acquired in the DFDP‐2B borehole yield the first continuous, subsurface description of the transition from schist to mylonite in the hangingwall of the Alpine Fault, New Zealand, to a depth of 818 m below surface. Thr
Externí odkaz:
https://doaj.org/article/91508e3f97cc4a35b8e9d5285a33f172
Publikováno v:
Solid Earth
New Zealand's Alpine Fault is a large, plate-bounding strike-slip fault, that ruptures in large (MW > 8) earthquakes. Its hazard potential is linked to its geometrical properties. We conducted field and laboratory analyses of fault rocks to elucidate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::566777c2ace3d192fdfebd6ac50c6aa4
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5000142_1/component/file_5000171/5000142.pdf
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5000142_1/component/file_5000171/5000142.pdf
Autor:
Jack N. Williams, Virginia G. Toy, Cécile Massiot, David D. McNamara, Steven A. F. Smith, Steven Mills
The orientations and densities of fractures in the foliated hanging-wall of the Alpine Fault provide insights into the role of a mechanical anisotropy in upper crustal deformation, and the extent to which existing models of fault zone structure can b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee1231ed2c330007cfea344bee5ba817
https://doi.org/10.5194/se-2017-112
https://doi.org/10.5194/se-2017-112
Publikováno v:
Journal of Structural Geology. 54:1-20
Publikováno v:
Environmental & Engineering Geoscience. 19:195-196