Activation of very low frequency earthquakes by slow slip events in the Ryukyu Trench [PDF]
AbstractLong‐term activity of shallow very low frequency earthquakes (VLFEs) in the Ryukyu Trench, unassociated with recent large thrust earthquakes, was analyzed using a broadband seismometer network. The distribution of shallow VLFEs was divided into three large clusters.
Mamoru Nakamura
exaly +2 more sources
Distribution of low-frequency earthquakes accompanying the very low frequency earthquakes along the Ryukyu Trench [PDF]
This study investigated the activity and distribution of low-frequency earthquakes (LFEs) accompanying the very low frequency earthquakes (VLFEs) in the central and southern Ryukyu Trench.
Mamoru Nakamura
doaj +2 more sources
Interchanges and movements of humpback whales in Japanese waters: Okinawa, Ogasawara, Amami, and Hokkaido, using an automated matching system. [PDF]
Humpback whales in the western North Pacific are considered endangered due to their small population size and lack of information. Although previous studies have reported interchanges between regions within a population, the relationship between the ...
Nozomi Kobayashi +13 more
doaj +2 more sources
We identified 27 new mud volcanoes, including potential ones, in a part of the Hyuga-nada area, southwest offshore Japan, at the northern end of the Ryukyu Trench, based on subseafloor geological structures using geophysical investigations.
Miho Asada +8 more
doaj +2 more sources
Episodic Slow Slip Events and Overlying Plate Seismicity at the Southernmost Ryukyu Trench
AbstractShallow slow slip events accompanied by seismicity has been increasingly reported in subduction zones during the last decade; however, the relationship between shallow slip events and seismicity is unclear. We report episodic slow slip events and seismicity at the southernmost Ryukyu Trench.
Sean Kuanhsiang Chen +2 more
exaly +2 more sources
A multidisciplinary Ocean Bottom Observatory (MDOBO) was installed on VENUS (Versatile Eco-monitoring Network by Undersea-cable System) a depth of 2,170 meters on the slope of the Ryukyu Trench.
Y. Shirasaki +6 more
doaj +5 more sources
Potential coupling of microbial methane, nitrogen, and sulphur cycling in the Okinawa Trough cold seep sediments [PDF]
The Okinawa Trough (OT) is a back-arc basin with a wide distribution of active cold seep systems. However, our understanding of the metabolic function of microbial communities in the cold seep sediments of the OT remains limited.
Ye Chen +10 more
doaj +2 more sources
Paleotsunami researches along the Ryukyu Trench
Kazuhisa Gotō
exaly +3 more sources
Slab Pull Drives IBM Trench Advance Despite the Weakened Philippine Sea Plate
The mechanism behind the significant Izu‐Bonin‐Mariana (IBM) trench advance is still controversial. We conduct slab subduction numerical models that reproduce the spatio‐temporal tectonic evolution of the Philippine Sea region to investigate whether slab
Huizi Jian +5 more
doaj +1 more source
Variations in the crustal structure and strength of plate coupling along the Ryukyu subduction zone
The Ryukyu trench-arc-back arc system is part of the subduction margins of the Philippine Sea plate. Previous studies have indicated that several geophysical and geological characteristics reveal significant variations (including convergent rate ...
Wen-Bin Doo +4 more
doaj +1 more source

