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The fate of fluids released from subducting slab in northern Cascadia
northern Cascadia subducting slab
2015/1/4
. Large amounts of water carried down in subduction zones are driven upward into the overlying forearc upper
mantle and crust as increasing temperatures and pressure dehydrate the subducting crust.
Constraining fault interpretation through tomographic velocity gradients: application to northern Cascadia
Constraining fault interpretation velocity gradients
2015/1/4
Spatial gradients of tomographic velocities are
seldom used in interpretation of subsurface fault structures.
This study shows that spatial velocity gradients can be used
effectively in identifying...
Constraining fault interpretation through tomographic velocity gradients: application to northern Cascadia
Constraining fault interpretation tomographic velocity gradients northern Cascadia
2015/1/4
Spatial gradients of tomographic velocities are seldom used in interpretation of subsurface fault structures. This study shows that spatial velocity gradients can be used effectively in identifying su...
The fate of fluids released from subducting slab in northern Cascadia
fluids released subducting slab northern Cascadia
2015/1/4
Large amounts of water carried down in subduction zones are driven upward into the overlying forearc upper mantle and crust as increasing temperatures and pressure dehydrate the subducting crust. Thro...