Subduction zone could generate strong stresses especially within subducting slab and also it makes special high pressure and low temperature environments. Ergo study on blueschist is important to understand active stresses in subduction zone and in addition to reveal geofluid circulations owing to abundant hydrous phases in it. Fabric analyses of naturally and experimentally deformed blueschists were investigated to delineate its implications for seismic anisotropy and source of seismicity in subducting oceanic crust.……広島大学(Hiroshima University)博士(理学)Sciencedoctora
The subduction interface is an inherently heterogeneous distributed shear zone occupying the boundar...
The subduction interface is an inherently heterogeneous distributed shear zone occupying the boundar...
International audienceFragments of ancient oceanic lithosphere preserved in mountain belts, though v...
Subduction zone could generate strong stresses especially within subducting slab and also it makes s...
AGU Fall Meeting 2021 Poster Presentation on the Seismic Anisotropy of Blueschists Abstract: Subdu...
To understand the causes of seismic low-velocity layers and seismic anisotropy of the subducting oce...
Many blueschists and eclogites are inferred to have formed from oceanic basalts in subducted slabs. ...
EBSD-based seismic anisotropy study of 14 naturally deformed epidote and lawsonite blueschists sourc...
International audienceUpon subduction, the oceanic crust transforms to blueschists and eclogites, wi...
International audienceUpon subduction, the oceanic crust transforms to blueschists and eclogites, wi...
We conducted a detailed study on the microstructures and petro-fabrics of massive and foliated lawso...
Along plate interfaces in subduction zones, displacement occurs by a spectrum of slip styles, inclu...
The origin of intermediate-depth seismicity has been debated for decades, because its formation at e...
The origin of intermediate-depth seismicity has been debated for decades, because its formation at e...
The origin of intermediate-depth seismicity has been debated for decades, because its formation at e...
The subduction interface is an inherently heterogeneous distributed shear zone occupying the boundar...
The subduction interface is an inherently heterogeneous distributed shear zone occupying the boundar...
International audienceFragments of ancient oceanic lithosphere preserved in mountain belts, though v...
Subduction zone could generate strong stresses especially within subducting slab and also it makes s...
AGU Fall Meeting 2021 Poster Presentation on the Seismic Anisotropy of Blueschists Abstract: Subdu...
To understand the causes of seismic low-velocity layers and seismic anisotropy of the subducting oce...
Many blueschists and eclogites are inferred to have formed from oceanic basalts in subducted slabs. ...
EBSD-based seismic anisotropy study of 14 naturally deformed epidote and lawsonite blueschists sourc...
International audienceUpon subduction, the oceanic crust transforms to blueschists and eclogites, wi...
International audienceUpon subduction, the oceanic crust transforms to blueschists and eclogites, wi...
We conducted a detailed study on the microstructures and petro-fabrics of massive and foliated lawso...
Along plate interfaces in subduction zones, displacement occurs by a spectrum of slip styles, inclu...
The origin of intermediate-depth seismicity has been debated for decades, because its formation at e...
The origin of intermediate-depth seismicity has been debated for decades, because its formation at e...
The origin of intermediate-depth seismicity has been debated for decades, because its formation at e...
The subduction interface is an inherently heterogeneous distributed shear zone occupying the boundar...
The subduction interface is an inherently heterogeneous distributed shear zone occupying the boundar...
International audienceFragments of ancient oceanic lithosphere preserved in mountain belts, though v...