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Strain and stress gradients through the backarc regions of Miocene western Japan: A new type of arc-parallel extension.

Authors :
Ushimaru, Kentaro
Yamaji, Atsushi
Source :
Journal of Structural Geology. Aug2023, Vol. 173, pN.PAG-N.PAG. 1p.
Publication Year :
2023

Abstract

The overriding lithosphere is occasionally stretched parallel to the consuming plate boundary. Such arc-parallel extension manifests itself mostly in forearc regions. Here, we report unique arc-parallel extension, which affected only the backarc regions with arc-parallel strain and stress gradients. The extension took place in the backarc regions of the northern Ryukyu and western SW Japan arcs in the Middle Miocene. The extension was evidenced by NW-SE trending normal faults in the extensional zone and paleostresses that were determined from dike orientations. To determine the age of and spatial extent of this zone, we analyzed fault-slip data from the Amakusa region, northern Ryukyu arc, where early middle Miocene intrusions allowed us to judge the magmatism to be older than the faults that affected Cretaceous and Eocene formations. The slip senses of the faults have been controversial in Amakusa. As a result, the region was found to have belonged to the extensional zone. The extensional zone is 300–400 km long and ∼100 km wide. We also found that the arc-parallel extension resulted in crustal strain with a southwestward increasing trend along the zone. The strain magnitudes showed a negative correlation with distance from the Okinawa Trough. This correlation is explained by the increasing stress magnitude toward the trough. We suggest that the stalled rift propagation of the northern Okinawa Trough caused the unique arc-parallel extension in the Middle Miocene. • Middle Miocene arc-parallel extension in the backarc regions of western Japan. • The extension followed widespread magmatism in the SW Japan and northern Ryukyu arcs. • Extensional strains in the regions had an increasing trend toward the Okinawa Trough. • No mechanism but a stress gradient though the regions account for the trend. • The gradient was caused by the stalled rift propagation in the Okinawa Trough. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
01918141
Volume :
173
Database :
Academic Search Index
Journal :
Journal of Structural Geology
Publication Type :
Academic Journal
Accession number :
169730812
Full Text :
https://doi.org/10.1016/j.jsg.2023.104894