The shallow tremors had similar migration properties to deep low - frequency tremors that occur at
the deep subducting plate interface, and that they also occurred synchronized in time and space with shallow very - low - frequency tremors that also thought to be triggered by slow slip events.
Not exact matches
Over long periods of time (think millions of years), the crust is
subducted deep into the mantle.
Using tomographic data, the authors inferred that the Caribbean plate crust to the north is
subducting at a very shallow angle and producing relatively little
deep seismicity.
Using GPS, InSAR, gravity, seismic reflection, and geological data, Marcos Moreno and colleagues from GFZ as well as Chile show that the 2016 earthquake occurred at the
deep boundary of a persistent asperity on the interface between the
subducting Nazca and overriding South American plates, where both plates are coupled and not sliding past each other in spite of the high convergence velocity of 68 mm / year.
Because such shifts in olivine change the structure of earth's
subducted lithosphere, the new phase transition mechanism could help explain the origins of some
deep earthquakes.
More perplexing still, seismic studies have shown no evidence that ocean crust is being
subducted — thrust down into the hot mantle underlying the trench — which is the process that results in quakes at other
deep - sea trenches.
As the
subducting plate sinks
deeper into the earth, it encounters higher and higher temperatures and pressures, which release the significant amount of water trapped in waterrich minerals that exist within the slab.
The broader region is vulnerable to earthquakes from multiple sources, including
deep earthquakes within the
subducted Juan de Fuca plate, offshore megathrust earthquakes on Cascadia subduction zone and the shallow crustal earthquakes within the North American Plate.
Hydration reactions along the
subducting plate are thought to carry water
deep into the Earth, and dehydration reactions at greater depths release fluids into the overlying mantle that promote melting and volcanism.
Deep earthquakes, also called intraplate quakes, take place within the oceanic Juan de Fuca plate (beneath Oregon and Washington) and the Gorda plate (beneath northwestern California) as they
subduct beneath the North America plate.
The logic is that it would have been
subducted as a function of plate tectonics billions of years ago, then encased in a forming diamond
deep in the mantle, and ultimately sent back up near the surface again.
However, it must be borne in mind that the MOC can also include shallower, wind - driven overturning cells such as occur in the upper ocean in the tropics and subtropics, in which warm (light) waters moving poleward are transformed to slightly denser waters and
subducted equatorward at
deeper levels.