Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.

Geologic Investigation of a Potential Site for a Next-Generation Reactor Neutrino Oscillation Experiment -- Diablo Canyon, San Luis Obispo County, CA

Autor: Onishi, Celia Tiemi, Dobson, Patrick, Nakagawa, Seiji, Glaser, Steven, Galic, Dom

Publikováno v: Onishi, Celia Tiemi; Dobson, Patrick; Nakagawa, Seiji; Glaser, Steven; & Galic, Dom. (2004). Geologic Investigation of a Potential Site for a Next-Generation Reactor Neutrino Oscillation Experiment--Diablo Canyon, San Luis Obispo County, CA. Lawrence Berkeley National Laboratory. Lawrence Berkeley National Laboratory: Lawrence Berkeley National Laboratory. Retrieved from: http://www.escholarship.org/uc/item/6830v26q
Onishi, Celia Tiemi; Dobson, Patrick; Nakagawa, Seiji; Glaser, Steven; & Galic, Dom. (2004). Geologic Investigation of a Potential Site for a Next-Generation Reactor Neutrino Oscillation Experiment--Diablo Canyon, San Luis Obispo County, CA. Lawrence Berkeley National Laboratory. Lawrence Berkeley National Laboratory: Lawrence Berkeley National Laboratory. Retrieved from: http://www.escholarship.org/uc/item/441098jr

This report provides information on the geology and selected physical and mechanical properties of surface rocks collected at Diablo Canyon, San Luis Obispo County, California as part of the design and engineering studies towards a future reactor neu

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::89fe9e33e270bd45c5299bfdaaceb554
http://www.escholarship.org/uc/item/6830v26q

Visualization of microcrack anisotropy in granite affected by a fault zone, using confocal laser scanning microscope

Autor: Onishi, Celia T., Shimizu, Ichiko

Publikováno v: Onishi, Celia T.; & Shimizu, Ichiko. (2004). Visualization of microcrack anisotropy in granite affected by a fault zone, using confocal laser scanning microscope. Lawrence Berkeley National Laboratory. Lawrence Berkeley National Laboratory: Lawrence Berkeley National Laboratory. Retrieved from: http://www.escholarship.org/uc/item/15g392zd

Brittle deformation in granite can generate a fracture system with different patterns. Detailed fracture analyses at both macroscopic and microscopic scales, together with physical property data from a drill-core, are used to classify the effects of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______325::78ef4328e6cf3efb9b5e55e38205ca8a
http://www.escholarship.org/uc/item/15g392zd

Change in fabric of melange in the Shimanto Belt, Japan: Change in relative convergence?

Autor: Onishi, Celia Tiemi, Kimura, Gaku

Publikováno v: Tectonics; 1995, Vol. 14 Issue 6, p1273-1289, 17p