[HTML][HTML] Marine cold seeps and their manifestations: geological control, biogeochemical criteria and environmental conditions

E Suess - International Journal of Earth Sciences, 2014 - Springer
Characteristics of cold seeps at different geologic settings are the subject of this review
primarily based on results of the Research Consortium SFB 574. Criteria are drawn from …

Marine cold seeps: background and recent advances

E Suess - Hydrocarbons, oils and lipids: Diversity, origin …, 2020 - Springer
Marine cold seeps are windows into different depth levels of the submerged geosphere.
Subduction zones and organic-rich passive margins host most of the world's cold seeps. The …

Real-time determination of earthquake focal mechanism via deep learning

W Kuang, C Yuan, J Zhang - Nature communications, 2021 - nature.com
An immediate report of the source focal mechanism with full automation after a destructive
earthquake is crucial for timely characterizing the faulting geometry, evaluating the stress …

Depth‐varying rupture properties of subduction zone megathrust faults

T Lay, H Kanamori, CJ Ammon… - Journal of …, 2012 - Wiley Online Library
Subduction zone plate boundary megathrust faults accommodate relative plate motions with
spatially varying sliding behavior. The 2004 Sumatra‐Andaman (Mw 9.2), 2010 Chile (Mw …

[HTML][HTML] Seafloor geodetic constraints on interplate coupling of the Nankai Trough megathrust zone

Y Yokota, T Ishikawa, S Watanabe, T Tashiro, A Asada - Nature, 2016 - nature.com
Interplate megathrust earthquakes have inflicted catastrophic damage on human society.
Such an earthquake is predicted to occur in the near future along the Nankai Trough off …

Tectonic and geological framework for gas hydrates and cold seeps on the Hikurangi subduction margin, New Zealand

PM Barnes, G Lamarche, J Bialas, S Henrys, I Pecher… - Marine Geology, 2010 - Elsevier
The imbricated frontal wedge of the central Hikurangi subduction margin is characteristic of
wide (ca. 150 km), poorly drained and over pressured, low taper (∼ 4°) thrust systems …

Frontal wedge deformation near the source region of the 2011 Tohoku‐Oki earthquake

Y Ito, T Tsuji, Y Osada, M Kido, D Inazu… - Geophysical …, 2011 - Wiley Online Library
We report an uplift of 5 m with a horizontal displacement of more than 60 m due to the 2011
Tohoku‐Oki earthquake. The uplift was measured by an ocean‐bottom pressure gauge …

Forearc basins: Types, geometries, and relationships to subduction zone dynamics

A Noda - Bulletin, 2016 - pubs.geoscienceworld.org
Forearc basins are one of the fundamental sedimentary basins, and they preserve various
geological phenomena arising from dynamic interactions between subducting and …

[HTML][HTML] Eastern Mediterranean tectonics and tsunami hazard inferred from the AD 365 earthquake

B Shaw, NN Ambraseys, PC England, MA Floyd… - Nature …, 2008 - nature.com
Historical accounts describe an earthquake and tsunami on 21 July ad 365 that destroyed
cities and drowned thousands of people in coastal regions from the Nile Delta to modern …

[PDF][PDF] Structural and seismic stratigraphic framework of the NanTroSEIZE Stage 1 transect

GF Moore, JO Park, NL Bangs, SP Gulick… - Proc. IODP …, 2009 - researchgate.net
The location of the Integrated Ocean Drilling Program's (IODP) Nankai Trough Seismogenic
Zone Experiment (NanTroSEIZE) was based on regional two-dimensional seismic reflection …