Zobrazeno 1 - 10
of 39
pro vyhledávání: '"William M. Dunne"'
Publikováno v:
Earth and Planetary Science Letters. 602:117928
Publikováno v:
Journal of Geophysical Research: Planets. 120:2053-2083
Fault dips are a function of the coefficient of internal friction, μi, of the lithospheric material. Laboratory deformation experiments of H2O ice at conditions applicable to icy bodies yield 0 ≤ μi ≤ 0.55 such that normal faults dip between 45
Publikováno v:
Journal of Structural Geology
Journal of Structural Geology, 2018, 108, pp.2-15. ⟨10.1016/j.jsg.2017.08.008⟩
Journal of Structural Geology, Elsevier, 2018, 108, pp.2-15. ⟨10.1016/j.jsg.2017.08.008⟩
Journal of Structural Geology, 2018, 108, pp.2-15. ⟨10.1016/j.jsg.2017.08.008⟩
Journal of Structural Geology, Elsevier, 2018, 108, pp.2-15. ⟨10.1016/j.jsg.2017.08.008⟩
International audience; Spatial arrangement is a fundamental characteristic of fracture arrays. The pattern of fault and opening mode fracture positions in space defines structural heterogeneity and anisotropy in a rock volume, governs how faults and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::af0a87cb34b4caeacf2954d2b66b9d8f
https://hal.science/hal-01765560/file/1_s2.0_S0191814117301621_main.pdf
https://hal.science/hal-01765560/file/1_s2.0_S0191814117301621_main.pdf
Publikováno v:
Journal of Geophysical Research: Solid Earth. 119:5979-5986
Data on fracture spacing along scan lines have been widely analyzed for the purposes of characterization. Most of these studies, however, either consider the cumulative frequency of spacing data without regard to the actual sequence of the spacing va
Publikováno v:
Journal of Structural Geology. 32:1444-1449
Previous studies on fracture networks have shown that fractures contained within distinct mechanical units (“stratabound”) are regularly spaced while those that terminate within the rock mass are clustered (“non-stratabound”). Lacunarity is a
Publikováno v:
Journal of Structural Geology. 108:1
Publikováno v:
Journal of Structural Geology. 31:960-971
Previous studies [O'Kane, A., Onasch, C.M., Farver, J., 2007. The role of fluids in low-temperature, fault-related deformation of quartz arenite. Journal of Structural Geology 29, 819--836; Cook, J., Dunne, W.M., Onasch, C.M., 2006. Development of a