Zobrazeno 1 - 10
of 15
pro vyhledávání: '"M. Yetton"'
Autor:
Garth Archibald, L. Richards, Mauri McSaveney, Chris Massey, Joseph Wartman, F. Della Pasqua, Anna Kaiser, L. Janku, Caroline Holden, M. Yetton
Publikováno v:
Landslides. 14:249-268
The 2010–2011 Canterbury earthquakes triggered many mass movements in the Port Hills including rockfalls, debris avalanches, slides and slumps, and associated cliff-top cracking. The most abundant mass movements with the highest risk to people and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32dce616163aa78411f22362b046c226
https://doi.org/10.1007/s10346-016-0684-8
https://doi.org/10.1007/s10346-016-0684-8
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
Publikováno v:
Bulletin of the New Zealand Society for Earthquake Engineering. 34:318-334
We present the main results of a probabilistic seismic hazard assessment of the Canterbury region recently completed for Environment Canterbury (formerly Canterbury Regional Council). We use the distribution of active faults and the historical record
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dbe0907336a1168afe2add133c051dc4
https://doi.org/10.5459/bnzsee.34.4.318-334
https://doi.org/10.5459/bnzsee.34.4.318-334
Autor:
M. Yetton, David C. Nobes
Publikováno v:
New Zealand Journal of Geology and Geophysics. 41:485-492
The Alpine Fault in central Westland is an oblique slip fault with a predominantly strike‐slip component of 25–35 mm/yr. The smaller vertical component has been variously estimated at between 5.5 and 14 mm/yr. Ground penetrating radar and level p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8760969eb657c965d6b5a1956fc78caa
https://doi.org/10.1080/00288306.1998.9514825
https://doi.org/10.1080/00288306.1998.9514825
Autor:
M. Yetton
Publikováno v:
New Zealand Journal of Geology and Geophysics. 41:475-483
Radiocarbon dates from trenching of the Alpine Fault trace at Crane Creek, between the Haupiri and Ahaura Rivers, demonstrate the last earthquake rupture at this location occurred between AD 1480 and 1645, with associated local river aggradation and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81199a6aa91535d98408e5b50293c15a
https://doi.org/10.1080/00288306.1998.9514824
https://doi.org/10.1080/00288306.1998.9514824
Autor:
Alan Cooper, John Beavan, B. Leitner, Richard J. Norris, Timothy A. Little, Susan Ellis, Ruth A. Harris, M. Yetton, Simon C. Cox, Mark Stirling, Kelvin Berryman, Laura M. Wallace, Stuart Henrys, Stephen Bannister, Donna Eberhart-Phillips, Jarg R. Pettinga, Rupert Sutherland, John Townend, Tim Stern
Publikováno v:
A Continental Plate Boundary: Tectonics at South Island, New Zealand
Geological observations require that episodic slip on the Alpine fault averages to a long-term displacement rate of 2-3 cm/yr. Patterns of seismicity and geodetic strain suggest the fault is locked above a depth of 6-12 km and will probably fail duri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3caf086736267bbb0f5df6880a7bfb12
https://doi.org/10.1029/175gm12
https://doi.org/10.1029/175gm12
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Publikováno v:
Scopus-Elsevier
The Canterbury region of the South Island of New Zealand straddles a wide zone of active earth deformation associated with the oblique continent-continent collision between the Australian and Pacific tectonic plates east of the Alpine fault. The asso
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d6806b2c6011a8f65a6bc6a57fa3cdde
http://www.scopus.com/inward/record.url?eid=2-s2.0-0035708569&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-0035708569&partnerID=MN8TOARS
Autor:
B. McKelvey, S. A. L. Read, P. Kingsbury, Garth Archibald, J. Muirson, Marlene Villeneuve, Chris Massey, H. Grant, G. D. Dellow, J. Kupec, M. Easton, C. Price, B. McDowell, J. Molloy, M. O’Halloran, Phil Glassey, P.J. Forsyth, Zane Bruce, A. Campbell, D. H. Bell, N. Traylen, G. De Pascale, M. Yetton, N. Perrin, I. McPherson, I. McCahon, D F Macfarlane, R. Van Dissen, R. Jongens, Dja Barrell, G. T. Hancox, I. Walsh, R. Green, Tim Davies, C. Gibbons
Publikováno v:
Scopus-Elsevier
Montanuniversität Leoben
Montanuniversität Leoben
At 12.51 pm (NZST) on 22 February 2011 a shallow, magnitude MW 6.2 earthquake with an epicentre located just south of Christchurch, New Zealand, caused widespread devastation including building collapse, liquefaction and landslides. Throughout the Po
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e4560f6d816fd4a2e68d4c4b4105909b
http://www.scopus.com/inward/record.url?eid=2-s2.0-84858855205&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-84858855205&partnerID=MN8TOARS
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.