Zobrazeno 1 - 10
of 25
pro vyhledávání: '"C. B. Raleigh"'
Autor:
C. B. Raleigh
Publikováno v:
Geophysical Journal of the Royal Astronomical Society. 14:113-118
Summary The observation that serpentinite becomes weak and brittle at its dehydration temperature provides an experimental basis for the hypothesis that mantle earthquakes are caused by shear fracturing where interstitial fluid pressure effectively r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::571ee20486be640c8d1aa2da3c21cb14
https://doi.org/10.1111/j.1365-246x.1967.tb06229.x
https://doi.org/10.1111/j.1365-246x.1967.tb06229.x
Autor:
C. B. Raleigh
Publikováno v:
Geophysical Journal of the Royal Astronomical Society. 14:45-49
Summary Several minerals which from their occurrence in nodular inclusions in basalts and on theoretical grounds are believed to occur in the upper mantle have been deformed experimentally at high temperature and pressure. The glide mechanisms on whi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bee2a5fea31cde7f3180234e642e5265
https://doi.org/10.1111/j.1365-246x.1967.tb06220.x
https://doi.org/10.1111/j.1365-246x.1967.tb06220.x
Publikováno v:
Flow and Fracture of Rocks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86b1c492305587ab6b5750c34453e5b6
https://doi.org/10.1029/gm016p0275
https://doi.org/10.1029/gm016p0275
Autor:
C. B. Raleigh
Publikováno v:
Journal of Geophysical Research. 73:5391-5406
Olivine deformed experimentally at 5-kb confining pressure undergoes plastic flow by slip on several systems. The active slip system is determined from microscopic study of slip bands, deformation lamellas and kink bands. At temperatures less than 10
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::acee4837dd07121785aa7c4274789208
https://doi.org/10.1029/jb073i016p05391
https://doi.org/10.1029/jb073i016p05391
Autor:
James L. Talbot, C. B. Raleigh
Publikováno v:
American Journal of Science. 265:151-165
Lamellar twinning on (100) and to a lesser extent on (001) are present in clinopyroxenes of deformed mafic and ultramafic rocks. Both sets of twins are mechanical in origin and form where the resolved shear stress on the twin-glide system is high. St
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::579fc39a4db61c72e0681e8a72be6bdd
https://doi.org/10.2475/ajs.265.2.151
https://doi.org/10.2475/ajs.265.2.151
Publikováno v:
Journal of Geophysical Research. 73:5439-5461
Olivine and pyroxene deformation in stony meteorites, noting texture variations with shock pressure
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c73bcc9fb230afc69e5701aa71604177
https://doi.org/10.1029/jb073i016p05439
https://doi.org/10.1029/jb073i016p05439
Publikováno v:
Science. 166:1467-1474
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9bfbc3b0ae8e27b99e927ada040df222
https://doi.org/10.1126/science.166.3912.1467
https://doi.org/10.1126/science.166.3912.1467
Publikováno v:
Science. 161:1301-1310
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ee50b18b4639da49cec92f67b846e183
https://doi.org/10.1126/science.161.3848.1301
https://doi.org/10.1126/science.161.3848.1301
Publikováno v:
Tectonophysics. 14:319-332
The San Andreas fault is viewed, according to the concepts of seafloor spreading and plate tectonics, as a transform fault that separates the Pacific and North American plates and along which relative movements of 2 to 6 cm/year have been taking plac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5802a2891bc4581ef84963cee16c0c7a
https://doi.org/10.1016/0040-1951(72)90080-7
https://doi.org/10.1016/0040-1951(72)90080-7
Autor:
Jean A. Minkin, Everett D. Jackson, O. B. James, E. C. T. Chao, C. B. Raleigh, Judith A. Boreman
Publikováno v:
Science. 167:644-647
On the basis of rock modes, textures, and mineralogy, unshocked crystalline rocks are classified into a dominant ilmenite-rich suite (subdivided into intersertal, ophitic, and hornfels types) and a subordinate feldspar-rich suite (subdivided into poi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a18ff6266d979b5412195ef455cddd7e
https://doi.org/10.1126/science.167.3918.644
https://doi.org/10.1126/science.167.3918.644