GEBCO gridded bathymetric datasets for mapping Japan trench geomorphology by means of GMT scripting toolset
P Lemenkova - Geodesy and Cartography, 2020 - papers.ssrn.com
The study investigated geomorphology of the Japan Trench located east of Japan, Pacific
Ocean. A high-resolution GEBCO Gridded Bathymetric Dataset was used for modeling …
Ocean. A high-resolution GEBCO Gridded Bathymetric Dataset was used for modeling …
The dynamics of unlikely slip: 3D modeling of low‐angle normal fault rupture at the Mai'iu fault, Papua New Guinea
Despite decades‐long debate over the mechanics of low‐angle normal faults (LANFs)
dipping less than 30°, many questions about their strength, stress, and slip remain …
dipping less than 30°, many questions about their strength, stress, and slip remain …
Both longitudinal and transverse extension controlling gas migration through submarine anticlinal ridges, New Zealand's southern Hikurangi margin
Sub‐seabed fluid flow, gas hydrate accumulation and seafloor methane seepage are tightly
interwoven processes with implications for marine biodiversity, ocean chemistry and …
interwoven processes with implications for marine biodiversity, ocean chemistry and …
Spatio-temporal distribution of shallow very-low-frequency earthquakes between December 2020 and January 2021 in Kumano-nada, Nankai subduction zone …
Y Yamamoto, K Ariyoshi, S Yada, M Nakano… - Earth, Planets and …, 2022 - Springer
We estimate the hypocenter locations and the centroid moment tensor solutions of the
shallow very-low-frequency earthquake (sVLFE) activity that occurred in the Kumano-nada …
shallow very-low-frequency earthquake (sVLFE) activity that occurred in the Kumano-nada …
In situ stress orientation from 3 km borehole image logs in the Koyna Seismogenic zone, Western India: implications for transitional faulting environment
Abstract Knowledge of the in situ stress regime is critical to investigate the genesis of
recurrent triggered seismicity over the past five decades in the Koyna seismogenic zone …
recurrent triggered seismicity over the past five decades in the Koyna seismogenic zone …
Arcuate stress state in accretionary prisms from real-scale numerical sandbox experiments
The stress states in accretionary prisms are important for understanding the building and
releasing of seismic energy. Numerous researchers have conducted sandbox experiments …
releasing of seismic energy. Numerous researchers have conducted sandbox experiments …
Three-dimensional topographic relief of the oceanic crust may control the occurrence of shallow very-low-frequency earthquakes in the Nankai Trough off Kumano
K Shiraishi, Y Yamada, M Nakano, M Kinoshita… - earth, planets and …, 2020 - Springer
To explore a local relationship between geological structures and the occurrence of very-low-
frequency earthquakes (VLFEs), a particular class of slow earthquakes with characteristic …
frequency earthquakes (VLFEs), a particular class of slow earthquakes with characteristic …
Spatial variation of shallow stress orientation along the Hikurangi Subduction Margin: Insights from in‐situ borehole image logging
Abstract Knowledge of the contemporary in‐situ stress orientations in the Earth's crust can
improve our understanding of active crustal deformation, geodynamic processes, and …
improve our understanding of active crustal deformation, geodynamic processes, and …
Spatial patterns in frictional behavior of sediments along the Kumano transect in the Nankai Trough
Fault slip activity at subduction zones is governed by sediment frictional properties, which in
turn are affected by diagenetic processes. To study the spatial patterns in frictional …
turn are affected by diagenetic processes. To study the spatial patterns in frictional …
Deformation of the Nankai Trough inner accretionary prism: The role of inherited structures
Accretionary prisms commonly grow seaward, with the strata of the inner prism consisting of
older, previously accreted outer prism rocks overlain by thick fore‐arc basin strata. We focus …
older, previously accreted outer prism rocks overlain by thick fore‐arc basin strata. We focus …