Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Gaye Downes"'
Publikováno v:
Seismological Research Letters. 88:342-353
A database of historical (preinstrumental) and modern (instrumentally recorded) tsunamis that have impacted or been observed in New Zealand has been compiled and published online. New Zealand’s tectonic setting, astride an obliquely convergent tect
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa5984c522aa676b6ac8ed867ad52bcf
https://doi.org/10.1785/0220160135
https://doi.org/10.1785/0220160135
Publikováno v:
Earth and Planetary Science Letters. 397:1-9
Tsunami earthquakes generate much larger tsunami than their surface wave magnitude would suggest and are a problem for tsunami warning systems. They are often not accompanied by intense or even strong ground shaking and hence do not provide a natural
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d218fc061d42450d0f135ab649c3f48c
https://doi.org/10.1016/j.epsl.2014.04.005
https://doi.org/10.1016/j.epsl.2014.04.005
Autor:
M Yetton, Gaye Downes
Publikováno v:
New Zealand Journal of Geology and Geophysics. 55:199-205
The 5 June 1869 (NZMT), 4 June 1869 (UT) Christchurch earthquake has long been known to have caused chimney and structural damage, to Modified Mercalli intensity MM7, in central Christchurch. On 31 August 1870, another strong earthquake shook the cit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75c0c165f6d47eca905342c1144eb604
https://doi.org/10.1080/00288306.2012.690767
https://doi.org/10.1080/00288306.2012.690767
Autor:
Lorena X. Cowan, Paul D. Grimwood, Kevin F. Fenaughty, Penny Leach, Elizabeth de J. Robertson, Jennifer M. Coppola, Gaye Downes
Publikováno v:
Seismological Research Letters. 81:984-991
New Zealand felt earthquake reports have been collected since the late 19th century. In March 2004, the GeoNet Project, operated by GNS Science, implemented an Internet-based questionnaire. The aim was to provide an objective and automatic assignment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::24f054fba9943464130921aaaa7ddd89
https://doi.org/10.1785/gssrl.81.6.984
https://doi.org/10.1785/gssrl.81.6.984
Autor:
Rodney Grapes, Gaye Downes
Publikováno v:
Journal of the Geological Society. 167:35-47
The geological effects of the 1855 Wairarapa New Zealand earthquake with an estimated magnitude of M w 8.2–8.4 provided Charles Lyell with direct evidence of the relationship between earthquakes, fault rupturing, regional uplift and subsidence. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::797b1ba3f83420a7d6e1f3078e21d843
https://doi.org/10.1144/0016-76492009-104
https://doi.org/10.1144/0016-76492009-104
Autor:
Graham S. Leonard, Rylee Pettersson, Douglas Paton, Robert Bell, David Johnston, Gaye Downes, Katharine Pishief
Publikováno v:
Kotuitui: New Zealand Journal of Social Sciences Online. 3:105-120
The magnitude 9.5 earthquake on 22 May 1960 in southern Chile was the largest instrumentally recorded earthquake in the 20th century. It generated a tsunami that swept the shores of Chile and radiated out across the Pacific, with the major loss of li
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::99f828eb1a4765c5bb713a7de4940058
https://doi.org/10.1080/1177083x.2008.9522436
https://doi.org/10.1080/1177083x.2008.9522436
Publikováno v:
Pure and Applied Geophysics. 164:547-564
We develop a probabilistic model for estimating the tsunami hazard along the coast of New Zealand due to plate-interface earthquakes along the South American subduction zone. To do this we develop statistical and physical models for several stages in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ea9a62b8d00bff082bef2e6e6ffb9ba
https://doi.org/10.1007/s00024-006-0166-3
https://doi.org/10.1007/s00024-006-0166-3
Publikováno v:
Bulletin of the New Zealand Society for Earthquake Engineering. 34:125-157
In 1942, two large earthquakes, on June 24 (Mw 7.2) and August 1 (UT) (Mw 6.8), strongly shook the lower North Island, causing widespread moderate to severe damage. A third earthquake (Ms 6.0) occurred in the same area on December 2. These earthquake
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1f4256f17ec9407406775163ee08795b
https://doi.org/10.5459/bnzsee.34.2.125-157
https://doi.org/10.5459/bnzsee.34.2.125-157
Publikováno v:
Bulletin of the New Zealand Society for Earthquake Engineering. 32:221-245
Descriptive accounts and analysis of local seismograms establish that the epicentre of the 1934 March 5 Ms7.6 earthquake, known as the Pahiatua earthquake, was nearer to Pongaroa than to Pahiatua. Conspicuous and severe damage (MM8) in the business c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b8674961db824e58cb34e9032dda024
https://doi.org/10.5459/bnzsee.32.4.221-245
https://doi.org/10.5459/bnzsee.32.4.221-245
Publikováno v:
New Zealand Journal of Geology and Geophysics. 41:387-399
Evidence from newspaper reports, diaries and journals, related first‐hand information, an 1854 survey map of the lower part of the Awatere Valley, and reports by geologists between 1856 and 1890, indicates that surface rupturing occurred on the Awa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a4b92bb364b47d9a6f62cd052e5c41c
https://doi.org/10.1080/00288306.1998.9514818
https://doi.org/10.1080/00288306.1998.9514818