Geodynamic controls on magmatic arc migration and quiescence
GM Gianni, SP Luján - Earth-Science Reviews, 2021 - Elsevier
Reconfigurations of magmatic arcs through time have been recognized since pioneering
works, describing inland and trenchward arc migrations or magmatic shut-off lasting for …
works, describing inland and trenchward arc migrations or magmatic shut-off lasting for …
Comparison of fold-thrust belts driven by plate convergence and gravitational failure
X Yang, FJ Peel, LC McNeill, DJ Sanderson - Earth-Science Reviews, 2020 - Elsevier
Deepwater fold-thrust belts (FTBs) are predominantly formed by the deformation of
sedimentary sequences as a result of subduction of oceanic plates at active margins …
sedimentary sequences as a result of subduction of oceanic plates at active margins …
Focused fluid seepage related to variations in accretionary wedge structure, Hikurangi margin, New Zealand
Hydrogeological processes influence the morphology, mechanical behavior, and evolution
of subduction margins. Fluid supply, release, migration, and drainage control fluid pressure …
of subduction margins. Fluid supply, release, migration, and drainage control fluid pressure …
Relating seafloor geomorphology to subsurface architecture: How mass‐transport deposits and knickpoint‐zones build the stratigraphy of the deep‐water Hikurangi …
Monitoring of modern deep‐water channels has revealed how migrating channel‐floor
features generate and remove stratigraphy, improving understanding of how channel …
features generate and remove stratigraphy, improving understanding of how channel …
Physical conditions and frictional properties in the source region of a slow-slip event
Recent geodetic studies have shown that slow-slip events can occur on subduction faults,
including their shallow (< 15 km depth) parts where tsunamis are also generated. Although …
including their shallow (< 15 km depth) parts where tsunamis are also generated. Although …
Temperature-dependent frictional properties of heterogeneous Hikurangi Subduction Zone input sediments, ODP Site 1124
Abstract The Hikurangi Subduction Zone (HSZ), New Zealand, accommodates westward
subduction of the Pacific Plate. Where imaged seismically, the shallow HSZ décollement (< …
subduction of the Pacific Plate. Where imaged seismically, the shallow HSZ décollement (< …
Sedimentation on structurally complex slopes: Neogene to recent deep‐water sedimentation patterns across the central Hikurangi subduction margin, New Zealand
AD McArthur, A Crisóstomo‐Figueroa, A Wunderlich… - Basin …, 2022 - earthdoc.org
Deep‐water sedimentation on active margins often entails complex sediment transport
pathways through slope accommodation. Sedimentation in such settings is commonly …
pathways through slope accommodation. Sedimentation in such settings is commonly …
Gas hydrate formation beneath thrust ridges: A test of concepts using 3D modelling at the southern Hikurangi Margin, New Zealand
Gas hydrates are widespread along convergent margins, but their distribution is highly
variable. This variability has been attributed to a range of factors, such as the source of gas …
variable. This variability has been attributed to a range of factors, such as the source of gas …
[HTML][HTML] The role of protothrusts in frontal accretion and accommodation of plate convergence, Hikurangi subduction margin, New Zealand
Protothrusts mark the onset of deformation at the toe of large subduction accretionary
wedges. They are recognized in seismic reflection sections as small-displacement (tens of …
wedges. They are recognized in seismic reflection sections as small-displacement (tens of …
Controls on the architectural evolution of deep-water channel overbank sediment wave fields: insights from the Hikurangi Channel, offshore New Zealand
Deep-water channels can be bound by overbank deposits, resulting from overspilling flows,
which are often ornamented with sediment waves. Here, high-resolution bathymetry …
which are often ornamented with sediment waves. Here, high-resolution bathymetry …