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 …

Terminal suturing between the Tarim Craton and the Yili‐Central Tianshan arc: Insights from mélange‐ocean plate stratigraphy, detrital zircon ages, and provenance …

N Abuduxun, W Xiao, BF Windley, Y Chen, P Huang… - …, 2021 - Wiley Online Library
New field relations and U‐Pb ages of detrital zircons from Middle Devonian‐Upper Triassic
sedimentary rocks in the South Tianshan constrain the time and style of terminal suturing …

The dynamics of forearc–back‐arc basin subsidence: Numerical models and observations from Mediterranean subduction zones

A Balázs, C Faccenna, T Gerya, K Ueda… - Tectonics, 2022 - Wiley Online Library
The subsidence history of forearc and back‐arc basins reflects the relationship between
subduction kinematics, mantle dynamics, magmatism, crustal tectonics, and surface …

Thermogenic methane and hydrogen generation in subducted sediments of the Nankai Trough

N Suzuki, K Koike, J Kameda, G Kimura - Communications Earth & …, 2024 - nature.com
Active and widespread CH4 accumulations and emissions in the Nankai Trough subduction
zone are attested by numerous mud volcanoes, gas plumes, and gas hydrates containing …

[HTML][HTML] Identification of the static backstop and its influence on the evolution of the accretionary prism in the Nankai Trough

T Tsuji, J Ashi, M Strasser, G Kimura - Earth and Planetary Science Letters, 2015 - Elsevier
To reveal the origin of a backstop and its influence on the evolution of the accretionary
prism, we analyzed reflection seismic data acquired in the Nankai Trough off the Kii …

Expedition 349 summary

CF Li, J Lin, DK Kulhanek, T Williams, R Bao, A Briais… - 2015 - boris.unibe.ch
C.-F. Li, J. Lin, DK Kulhanek, T. Williams, R. Bao, A. Briais, EA Brown, Y. Chen, PD Clift, FS
Colwell, KA Dadd, W.-W. Ding, I. Hernández-Almeida, X.-L. Huang, S. Hyun, T. Jiang, AAP …

Middle Miocene renewed subduction of arabian-eurasian plates: Implications for convergent tectonic mechanisms, tectonically-induced fluid overpressures, and …

U Khan, M Khan, S Wu, G Jinwei - Marine and Petroleum Geology, 2024 - Elsevier
The complex interplay between thrust wedge deformation, tectonically-induced fluid
overpressures, and the complex phases of wedge-top sedimentary depositional systems in …

Punctuated growth of an accretionary prism and the onset of a seismogenic megathrust in the Nankai Trough

G Kimura, H Koge, T Tsuji - Progress in Earth and Planetary Science, 2018 - Springer
Ocean drilling in the Nankai Trough forearc suggests a new scenario for the evolution of the
Nankai subduction zone. Continuous subduction since the Late Cretaceous has been a …

Deposition and deformation of modern accretionary-type forearc basins: Linking basin formation and accretionary wedge growth

A Noda, A Miyakawa - … Models of Convergent Margins-Origin of …, 2017 - books.google.com
Since a comprehensive review of forearc basins was published by Dickinson more than 20
years ago, a significant amount of new data about them have been published. These recent …

Age and provenance of the Nindam Formation, Ladakh, NW Himalaya: evolution of the Intraoceanic Dras Arc before collision with India

JMJ Walsh, S Buckman, AP Nutman, R Zhou - Tectonics, 2019 - Wiley Online Library
Abstract The Dras Arc in NW India Himalaya is a belt of basaltic‐andesites intercalated with
arkose‐dominated volcaniclastic rocks of the Nindam Formation situated along the Indus …