The GPS network detected the slow slip events occurring on the Hikurangi
subduction zone plate boundary in the weeks and months following the Kaik?ura earthquake.
Not exact matches
SASMEX's main focus is on earthquakes originating in the
subduction zone off the southern coast of Mexico, where the Cocos tectonic
plate subducts below the North American P
plate subducts below the North American
PlatePlate.
They simulated earthquakes with magnitudes between 9.0 and 9.6 originating at different locations along the Aleutian - Alaska
subduction zone, a 3,400 - kilometer (2,113 - mile) long ocean trench stretching along the southern coast of Alaska and the Aleutian Islands where the Pacific tectonic
plate is slipping under the North American
plate.
Three basic forces are believed to drive oceanic
plate movement:
plates are «pushed» away from mid-ocean ridges as new sea floor forms;
plates are «pulled» as the oldest parts of the
plate dive back into the earth at
subduction zones; and convection within the asthenosphere helps ferry the
plates along.
The pressure difference could be caused by hot, partially molten rock piled up beneath mid-ocean ridges or beneath the cooling
plates diving into the earth at
subduction zones, the authors write.
One hint of weak coupling at a
subduction zone is the presence of serpentinite — a mineral formed when seawater carried down by a descending
plate reacts with mantle rock.
Many of the islands sit above a
subduction zone, where two
plates meet and one slides haltingly under the other, down into the Earth's mantle.
«Measuring the strength of olivine is critical to understanding how strong tectonic
plates are, which, in turn, matters to how
plates break and create
subduction zones like those along the Cascadia
plate, which runs down the west coast of Canada to the west coast of the United States,» said Warren, a geologist in the College of Earth, Ocean, and Environment.
On the Pacific Coast, this area sits along the
subduction zone known as the Cascadia
plate, which runs down the west coast of Canada to the west coast of the United States.
The Earth's lithosphere is divided into several
plates that are in constant motion, and today's geologists have a good understanding of what drives these
plate movements: heavier ocean
plates are submerged beneath lighter continental
plates along what are known as
subduction zones.
Events of this magnitude normally occur in a
subduction zone, where one tectonic
plate slides beneath another.
But just as in the past, earth scientists still do not understand what triggered
plate tectonics in the first place, nor how the first
subduction zone was formed.
The island nation sits atop an active
subduction zone where the Pacific
Plate slips below the Australian
Plate.
Most earthquakes are said to occur at
subduction zones or along faults in tectonic
plates.
The ocean
plate is descending below North America at the Cascadia
subduction zone, which runs from northern Vancouver Island, British Columbia, to Northern California.
The Tohoku - Oki earthquake occurred in a «
subduction zone,» a boundary between two tectonic
plates where one
plate is diving beneath another — in this case, the Pacific
plate dives beneath the Eurasian
plate just east of Japan.
The billion - year time lag between the earliest, «proto -
subduction» and the full onset of
plate tectonics can be explained by the slow, painstaking development of weak
zones within the
plates, he proposes.
The strain that is released in a
subduction zone earthquake is thought to build up in the deep portion of the fault where the two
plates are «locked.»
«Orogenic oceanic - continental
subduction zones have been common as long as modern
plate tectonics have been active,» Delph said.
In these regions of «flat - slab»
subduction, the Nazca
plate moves horizontally for several hundred kilometers before continuing its descent into the mantle, and is shadowed by an extended
zone of crustal seismicity in the overlying South America
plate.
Instead, the new finding adds evidence that gravity pulling the
plates into
subduction zones may drag them across the globe.
The map shows that, so far, almost all of the aftershocks have occurred along the
subduction zone that lies on the boundary of the Pacific
plate.
The Sea of Okhotsk earthquake may have involved re-rupture of a fault in the
plate produced when the oceanic
plate bent down into the Kuril - Kamchatka
subduction zone as it began to sink.
With these
plate tectonic reconstructions Schellart was able to predict where the fossil
subduction zone was during its lifetime some 50 - 70 million years ago, and therefore where the lithospheric slab disappeared into the mantle.
This regularity could shed light on the workings of tectonic
plate boundaries called
subduction zones, and it might even turn out to herald a season of heightened risk for larger quakes.
At
subduction zones such as these, an oceanic tectonic
plate sinks (subducts) into the Earth's interior, the mantle.
The deep mantle - derived buoyancy, together with
plate cooling at the surface, creates negative buoyancy that together explain the observations along the East Pacific Rise and surrounding Pacific
subduction zones.
(A
subduction zone is where one tectonic
plate sinks below another.)
Ward modeled the effects of a magnitude 9.2 earthquake in the Cascadia
subduction zone — a 58,000 - square - mile region in the Pacific from British Columbia to Northern California where the Juan de Fuca
plate sinks beneath the North American
plate.
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 P
plate, offshore megathrust earthquakes on Cascadia
subduction zone and the shallow crustal earthquakes within the North American
PlatePlate.
The team will focus on the Sunda
subduction zone, where the Indo - Australian
plate goes beneath the Sunda
plate.
At certain
subduction zones, such as those in Cascadia, Sumatra and eastern Alaska, a thick sediment layer overlies the subducting oceanic
plate.
The project «offers a unique opportunity to image the seismic structures associated with an entire
plate, including its spreading center and
subduction zone, within an easily accessible part of the continental and offshore United States,» said University of Massachusetts Amherst researcher Haiying Gao, a guest editor of the SRL focus section.
Subduction zones are areas where one tectonic
plate dives or «subducts» beneath another
plate.
Scientists have long thought diamonds could form in
subduction zones, where one tectonic
plate plunges under another and sinks hundreds of kilometers into the mantle.
The Sea of Okhotsk rests above a
subduction zone, a place where one of the Earth's tectonic
plates slides beneath another.
Both events occurred along a
subduction zone, an area where a tectonic
plate dives or «subducts» beneath an adjacent tectonic
plate.
The Arabian and Eurasian tectonic
plates collide offshore of Pakistan, forming a
subduction zone, but today's earthquake was onshore and mostly strike - slip — each side of the fault moved horizontally.
From the time interval (56 years), the known speed of the Nazca
plate, and further knowledge of the
subduction zone, the German - Chilean team has calculated the accumulated energy and thus the theoretical slip of the 2016 earthquake to about 3.4 meters.
The earthquake occurred along a 500 - kilometre segment of the Peru - Chile
subduction zone, where part of the Nazca
Plate in the Pacific Ocean plunges beneath the South American
Plate.
A
plate can bump up against another
plate at a fault
zone, or dive beneath one at a
subduction zone.
The volcanoes are formed by conditions at the
subduction zone where one of Earth's largest tectonic
plates, the Pacific
Plate, dives beneath the Australian
Plate.
The
subduction zone along the western edge of South America, where the Nazca
plate slides eastward beneath the South American
plate at an average rate of about 6.5 centimeters per year, can indeed generate massive quakes.
«We are interested in large - scale geophysical processes, like how
plate tectonics initiates and how
plates move underneath one another in
subduction zones,» said David Goldsby, an associate professor at the University of Pennsylvania.
In a
subduction zone, a heavy oceanic
plate meets a second, lighter continental
plate and moves under it and into the earth's mantle.
In high - pressure and high - temperature X-ray measurements that were partly conducted at DESY, scientists created conditions similar to those in so - called
subduction zones where an oceanic
plate dives under the continental crust.
Because it lies just slightly west of the Cascadia
subduction zone, the young seafloor is easily shoveled east beneath the North American
Plate.
Such a fracture, says Duarte, is evidence of an «embryonic
subduction zone,» where a new edge is formed, then forced under the remainder of the
plate, into the Earth's molten mantle.
For example, waves move slower when passing through hot magma, such as mantle plumes and hotspots, than they do when passing through colder
subduction zones, locations where one tectonic
plate slides beneath another.
The study, published February 12 in Nature Geoscience, focused on the Costa Rica
subduction zone where the Cocos
plate slowly dives beneath the overriding Caribbean
plate.