Northern Kyushu, characterized by the subduction of two oceanic slabs (a hot Shikoku basin and a cold Philippine Sea plate) beneath the Eurasian plate, forms a complex portion of Southwestern Japan arc. In order to evaluate the effect of slab-derived fluids from these two contrasting oceanic ...
aDeclarations in Plan over 声明在计划[translate] afroth floatation 泡沫漂浮[translate] acommonly used E-mail 常用的电子邮件[translate] athe subduction of the Pacific and Philippine Sea Plates beneath Eurasia 和平和菲律宾海板材的算术的减法在欧亚大陆之下[translate]...
The northernmost converging boundary of the Philippine Sea (PHS) plate crosses the base of the Izu Peninsula about 60 km southwest of Tokyo, subducting beneath Japan, a part of the Eurasian (EUR) plate. The 1923 Kanto earthquake ( M s =... K Nakamura,K Shimazaki,N Yonekura - 《Tectonophy...
Typical high electrical conductivity (0.1~1 S/m) regions associated with subduction zones, These regions include the Chile-Bolivia region5, the Philippine Sea6, the Cascadia Oregon7, the areas of Kyushu, Japan8 and North Honshu, Japan9, and Mount Rainier, USA10. Full size image Serpentine...
Shimakawa Y, Honkura Y: Electrical conductivity structure beneath the Ryukyu trench-arc system and its relation to the subduction of the Philippine sea plate.J Geomagnetism Geoelectricity1991, 43: 1–20. ArticleGoogle Scholar Soyer W, Unsworth M: Deep electrical structure of the northern Cascadia...
We show that the dense, high-rigidity Kumano pluton generates a large vertical load, which forces the incoming Philippine Sea Plate to subduct with a trajectory that is a factor of two steeper than adjacent regions. Beneath the region of maximum curvature and faulting of the Philippine Sea ...
The OLD is caused by plate subduction resulted from the mantle convection, and is an active fast delamination. 大洋岩石圈拆沉是由板块俯冲引起的,是地幔对流的产物,因此是一种快速的主动的拆沉; Subduction zones are the sites of oceanic trenches, high earthquake activity, and most of the world's ...
We suggest that low plate coupling may facilitate the uplifting of serpentinized mantle material up to the plate boundary. Introduction The Taiwan orogen, one of the world’s most active mountain belts, is shaped by the collision between the Philippine Sea plate (PSP) and the Eurasian plate (...
The Nankai Trough, formed by the northwestward subduction of the Philippine Sea Plate (PHP in Fig. 1) beneath the Eurasian plate at approximately 4 cm/year (e.g., Seno et al. 1993), is a plate boundary where earthquakes of magnitude 8 have occurred at intervals of 100–200 years (e....
The subduction of the Pacific and Philippine plates has led to a complex effect on the eastern part of the continent. In Northeast and North China, the E-W-directed stress is dominated by compression due to the compression of the ocean plate and the obstacle of the block to the north. ...