Zobrazeno 1 - 10
of 66
pro vyhledávání: '"A. R. Orpin"'
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 16, Iss 5, Pp 1239-1257 (2016)
Devastating tsunami over the last decade have significantly heightened awareness of the potential consequences and vulnerability of low-lying Pacific islands and coastal regions. Our appraisal of the potential tsunami hazard for the atolls of the Tok
Externí odkaz:
https://doaj.org/article/992fbc841fcd4ea09fd4914e0619d75c
Autor:
Katharine T. Bigham, Daniel Leduc, Ashley A. Rowden, David A. Bowden, Scott D. Nodder, Alan R. Orpin
Publikováno v:
PeerJ, Vol 12, p e17367 (2024)
Turbidity flows can transport massive amounts of sediment across large distances with dramatic, long-lasting impacts on deep-sea benthic communities. The 2016 Mw 7.8 Kaikōura Earthquake triggered a canyon-flushing event in Kaikōura Canyon, New Zeal
Externí odkaz:
https://doaj.org/article/cfaa72fff66d48399e0b8e46537e39a7
Autor:
Katharine T. Bigham, Ashley A. Rowden, David A. Bowden, Daniel Leduc, Arne Pallentin, Caroline Chin, Joshu J. Mountjoy, Scott D. Nodder, Alan R. Orpin
Publikováno v:
Frontiers in Marine Science, Vol 10 (2023)
Sediment density flows are large scale disturbances that can have dramatic impacts on seafloor animal communities in the deep sea. Seafloor imagery collected in Kaikōura Canyon (New Zealand), before and after a sediment density flow event that inclu
Externí odkaz:
https://doaj.org/article/6b913f1bd82e490f80943868b48514ce
Publikováno v:
New Zealand Journal of Geology and Geophysics. 66:42-58
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::84015c273c17d593c5ddbdfa77f28ca7
https://doi.org/10.1080/00288306.2021.2011328
https://doi.org/10.1080/00288306.2021.2011328
Autor:
Yoshihiro Kaneko, Jamie Howarth, Scott D. Nodder, M. Namık Çağatay, Philip M. Barnes, Helen C Bostock, Alan R. Orpin, Caroline Holden, Lorna J. Strachan, Katie Jones, Joshu J. Mountjoy
Publikováno v:
Nature Geoscience. 14:161-167
Turbidite palaeoseismology has produced arguably the most comprehensive multimillennial scale records of subduction-zone earthquakes but is underpinned by techniques that are vigorously debated in earthquake science. Resolving this argument requires
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7eca2c681d050217b53673a771985ce
https://doi.org/10.1038/s41561-021-00692-6
https://doi.org/10.1038/s41561-021-00692-6
This is the articlesSupplementary Appendix 1. Measured foraminiferal data for 2016 Kaikōura turbidite samples used in analyses. It contains information on all the foraminiferal samples studied from the 2016 turbidite in cores at bathyal and abyssal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40638e34837f71b94b0b0e892b713850
This is the first of a two-part New Zealand Journal of Geology and Geophysics Special Issue that focuses on improving our understanding of sedimentary systems of the Hikurangi Subduction Margin, Aotearoa-New Zealand. It is amongst the world’s young
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fbe5c0839a71de2d96d5a1f8ac8a40be
Autor:
Bruce W. Hayward, Ashwaq T. Sabaa, Jamie D. Howarth, Alan R. Orpin, Lorna J. Strachan, Stephanie E. Tickle
Publikováno v:
Marine Micropaleontology. 176:102171
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dd065bf3bb1c792d23a1ba682f7d7fae
https://doi.org/10.1016/j.marmicro.2022.102171
https://doi.org/10.1016/j.marmicro.2022.102171
To better understand earthquake reoccurrence and hazard, records of ancient earthquakes spanning millennia are routinely generated using seabed turbidite deposits, inferred to be synchronously triggered by strong ground motions over large geographic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62a74bac35ff6c3712b2c02b7c27b4dc
https://doi.org/10.5194/egusphere-egu2020-21034
https://doi.org/10.5194/egusphere-egu2020-21034
Autor:
John Mitchell, Geoffroy Lamarche, Tim Kane, Ashley A. Rowden, S Watson, Helen L. Neil, Alan R. Orpin, Gareth Crutchley, Ingo Pecher, Philip M. Barnes, David A. Bowden, Aaron Micallef, Jess I. T. Hillman, Arne Pallentin, Susi Woelz, Joshu J. Mountjoy, Ben Higgs
Hydrogeological processes influence the morphology, mechanical behavior, and evolution of subduction margins. Fluid supply, release, migration, and drainage control fluid pressure and collectively govern the stress state, which varies between accreti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::10ad0f53ce8da44abaa38e2c65f1d6fc