Zobrazeno 1 - 4
of 4
pro vyhledávání: '"E. G. C. Smith"'
Autor:
D. N. Jennings, R. T. Hefford, E. B. Lapish, R. I. Skinner, J. Hunt, T. W. Robertson, H. E. Chapman, E. G. C. Smith, H. W. Wellman, M. D. Gillon, B. J. Davidson, W. J. Cousins, G. H. McVerry, L. T. Pham, P. D. Leslie, D. G. Pemberton, J. B. Berrill, R. J. W. Granwal, A. G. Smaill, G. C. Clifton, R. C. Cooney, A. J. Macdonald, J. L. Morrison, B. W. Riddolls, J. N. O. Coad, A. L. Rutledge, Michael Pender, C. O'Brien, G. A. Salt
Publikováno v:
Earthquake Spectra. 3:659-745
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::245c8ebb2e15476383fd387dbcd871e4
https://doi.org/10.1193/1.1585452
https://doi.org/10.1193/1.1585452
Autor:
T. M. Hunt, E. G. C. Smith
Publikováno v:
Journal of the Royal Society of New Zealand. 12:159-180
Values are given for the magnetisation of thirteen groups of igneous rocks from New Zealand: 2 rhyolites, 1 ignimbrite, 1 trachyte, 2 andesites, 6 basalts and 1 peridotite; and ranging in age from Permian:Jurassic to Quaternary. Values of intensity o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d8fe4eac8ae6cfaff69a4212b151f8ba
https://doi.org/10.1080/03036758.1982.10419438
https://doi.org/10.1080/03036758.1982.10419438
Autor:
H. Anderson, E. G. C. Smith
Publikováno v:
Bulletin of the New Zealand Society for Earthquake Engineering. 22:2-38
The workshop was held in Wellington on September 19 and 20, 1988. It was preceded by a field trip on September 18 to look at the evidence of recent movements on the Wairarapa Fault, and followed by a similar trip to sites on the Wellington Fault on S
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7958269da1c0c4f11543baf7e8f93f09
https://doi.org/10.5459/bnzsee.22.1.2-38
https://doi.org/10.5459/bnzsee.22.1.2-38
Autor:
E. G. C. Smith
Publikováno v:
New Zealand Journal of Geology and Geophysics. 22:473-478
The distribution of micro-earthquakes observed in a 17 day survey of the Rangitikei-Manawatu region in February 1977, was similar to the long-term earthquake distribution. From the spatial distribution of the micro-earthquakes observed, it is conclud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be09882cc76746a3ec20495b035e6987
https://doi.org/10.1080/00288306.1979.10424155
https://doi.org/10.1080/00288306.1979.10424155