Zobrazeno 1 - 10
of 1 159
pro vyhledávání: '"Hikurangi"'
Autor:
Goutami Das, Saumen Maiti
Publikováno v:
Energy Geoscience, Vol 5, Iss 2, Pp 100227- (2024)
Pore pressure (PP) information plays an important role in analysing the geomechanical properties of the reservoir and hydrocarbon field development. PP prediction is an essential requirement to ensure safe drilling operations and it is a fundamental
Externí odkaz:
https://doaj.org/article/f50d08a9afd94ab68660b9cd7bf43120
Autor:
Nicola Tisato, Carolyn D. Bland, Harm VanAvendonk, Nathan Bangs, Hector Garza, Omar Alamoudi, Kelly Olsen, Andrew Gase
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 2, Pp n/a-n/a (2024)
Abstract Fluid flow and pore‐pressure cycling are believed to control slow slip events (SSEs), such as those that frequently occur at the northern Hikurangi margin of New Zealand. To better understand fluid flow in the forearc system we examined th
Externí odkaz:
https://doaj.org/article/36d796daf33d48ef947c8830e75182ac
Autor:
George D.F. Wilson
Publikováno v:
European Journal of Taxonomy, Vol 917, Iss 1 (2024)
A new family-level taxon of deep-sea isopods, Basoniscus hikurangi gen. et sp. nov., was recovered from the Hikurangi Plateau in the deep sea off eastern New Zealand. The broad-bodied, eyeless, seemingly unremarkable isopod was unusual in its possess
Externí odkaz:
https://doaj.org/article/71b1ce809c3f4d81977a943588d56824
Autor:
Dan Bassett, Gou Fujie, Shuichi Kodaira, Ryuta Arai, Yojiro Yamamoto, Stuart Henrys, Dan Barker, Andrew Gase, Harm vanAvendonk, Nathan Bangs, Hannu Seebeck, Brook Tozer, Katie Jacobs, Thomas Luckie, David Okaya, Kimi Mochizuki
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 22, Pp n/a-n/a (2023)
Abstract Marine multichannel and wide‐angle seismic data constrain the distribution of seamounts, sediment cover sequence and crustal structure along a 460 km margin‐parallel transect of the Hikurangi Plateau. Seismic reflection data reveals five
Externí odkaz:
https://doaj.org/article/6a2ada0199ea4c0c84810688016e484b
Akademický článek
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Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 3, Pp n/a-n/a (2023)
Abstract Slow slip events in the northern Hikurangi margin of Aotearoa New Zealand occur every 18–24 months and last for several weeks before returning to average convergence rates of around 38 mm/yr. Along this plate boundary, the Hikurangi platea
Externí odkaz:
https://doaj.org/article/c108c91fac524d55b8ad1ef224724d5d
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Theoretical studies of the seismic cycle at convergent plate boundaries anticipate that most coseismic deformation is recovered, yet significant permanent vertical displacement of the overriding plate is observed at many subduction margins. To unders
Externí odkaz:
https://doaj.org/article/40a46b622e53421c8572fe9ed279796e
Publikováno v:
Remote Sensing, Vol 15, Iss 19, p 4767 (2023)
Slow slip events (SSEs) are geophysical phenomena primarily occurring in subduction zones. These events are often associated with seismic activity and can be detected by Global Positioning System (GPS). However, the relationship between SSEs and seis
Externí odkaz:
https://doaj.org/article/c383e45fb9d74ac8b232b0a4faf94662
Publikováno v:
Journal of Marine Science and Engineering, Vol 11, Iss 7, p 1359 (2023)
The Tuaheni Landslide Complex, located on the upper slope of the northern Hikurangi Margin in New Zealand, is a unique place to research on slow slip creep-like deformation and seabed failure, as well as their possible relationship with the presence
Externí odkaz:
https://doaj.org/article/1de5849fc2db445aaf0342efe9f6e1ee
Akademický článek
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