「Subduction」の共起表現(1語右で並び替え)

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共起表現

「Subduction」の共起表現一覧(1語右で並び替え)

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future in Sumatra because of its continuous	subduction activity.
nt volcanoes that have formed as a result of	subduction along the Aleutian Trench.
The rising buoyant plutons resulted from	subduction along what was then the west coast of North
gone a complex process of plate convergence,	subduction, and arc volcanism from the Middle Eocene to
nic crust, it is cool at the time of initial	subduction and so is carried down to into the mantle.
	Subduction at the Tethyan Trench probably caused the co
cean) developed in the Neoproterozoic Era by	subduction at the expense of the global Mirovia ocean.
rthquake along the Cotabato Trench region of	subduction being the March 6, 2002 earthquake in Southe
rld, and occurs in a geologic setting of the	subduction belt of Namibia, which produces the conditio
iak Seamount will eventually be destroyed by	subduction by the Aleutian Trench once it is carried in
cian by island arc volcanic activity, due to	subduction during the closing of the Iapetus Ocean.
The	subduction interface around this region include the Nan
he earthquake was caused by a rupture of the	subduction interface.
Retrograde	subduction is interpreted to occur at the circular arc
Although	subduction no longer occurs between these two plates, t
The	subduction of the Charcot Plate stopped before 83 Ma, a
s an arcuate tectonic feature related to the	subduction of the African Plate beneath the Aegean Sea
e around 730 million years ago with eastward	subduction of the Tilemsi arc, which was accreted again
id that these earthquakes were caused by the	subduction of the Molucca Sea Plate.
The magmatic zone was formed by	subduction of oceanic crust along a pre-existing contin
contains transverse scars indicating earlier	subduction of seamounts.
f Ecuador is dominated by the effects of the	subduction of the Nazca Plate beneath the South America
earthquake occurred as a result of the past	subduction of the Australia Plate beneath the Timor Pla
f mainly extensional tectonics caused by the	subduction of the African Plate beneath Aegean Sea Plat
c formed 57 million years ago as a result of	subduction of the eastern block of the Kula Plate endin
e a result of thrust-faulting, caused by the	subduction of the Nazca plate beneath the South America
s an arcuate tectonic feature related to the	subduction of the African Plate beneath the Aegean Sea
rallel to the Nankai Trough, which marks the	subduction of the Philippine Sea Plate beneath the Eura
land arcs pushed upward by the collision and	subduction of tectonic plates.
lurian to the Pleistocene as a result of the	subduction of the Philippine Sea Plate beneath the cont
ic region is thought to be the result of the	subduction of the Tehuantepec Ridge, an undersea ridge
south, with east-west compression due to the	subduction of the Farallon slab beneath western North A
ly East-West compression that was due to the	subduction of the Farallon plate under western North Am
ontinental uplift in response to the shallow	subduction of the Farallon Plate.
	Subduction of the Kula Plate ceased after the creation
of heat for volcanism in the Lassen area is	subduction off the Northern California coast of the Gor
Such UHP metamorphic rocks record	subduction or continental collisions in which crustal r
Many are created by continental volcanic arc	subduction or the collision of sialic masses.
Some authors believe that the	subduction process is still ongoing.
s are converted back to silicates during the	subduction process.
ting, continental collisions, unroofing, and	subduction roll-back.
They can be produced by slip along the	subduction thrust fault or slip on faults within the do
aribbean Plate and was formed by the plate's	subduction under the South American Plate.
e authors have suggested alternate styles of	subduction, while others attribute the development of T
are thought to be related to Farallon plate	subduction, while the later bimodal assemblage (especia
stopped subducting under North America; the	subduction zone moved to the Farallon Trench further we
rmation of this fault zone is related to the	subduction zone in the west of Sumatra.
This former	subduction zone is now the Beringian Margin, which now
kaline arc volcanism that developed over the	subduction zone of the flysch basins.
There was a	subduction zone on the Slide Mountain Oceans floor call
It represents the part of the	subduction zone where the thick oceanic Hikurangi Plate
Mountain Ocean the Bridge River Ocean had a	subduction zone on the ocean floor called the Insular T
earthquakes on record, ruptures the Cascadia	subduction zone offshore from Vancouver Island to north
of an active volcanic arc, formed above the	subduction zone where the Indo-Australian Plate passes
faulting at a high angle to the trend of the	subduction zone and it has been suggested that the caus
ssibly induced by (and therefore close to a)	subduction zone and possibly in an island arc setting.
he Nankai Trough, a highly active, vigorous,	subduction zone where large earthquakes have been recor
ed; their chemistry is similar to modern-day	subduction zone magmas, but there is disagreement as to
nd Tonga Trenches represent the parts of the	subduction zone where oceanic crust of the Pacific Plat
ciated with a complex transition between the	subduction zone to the south along the Lesser Antilles
The major slip events on the	subduction zone interface are typically of megathrust t
The	subduction zone separates the Juan de Fuca, Explorer, G
of seismicity and volcanic eruptions, with a	subduction zone and many faults.
So scientifically speaking, the actual	subduction zone itself has not ruptured in almost 300 y
w Zealand's North Island (see Kermadec-Tonga	Subduction Zone).
form part of the island arc formed above the	subduction zone, where the Pacific Plate is being subdu
ude that the fault zone here is an incipient	subduction zone, with oblique motion corresponding to t
cement is mainly taken up along the Kermadec	subduction zone, although the remaining dextral strike-
is mainly taken up along the Kermadec-Tonga	subduction zone, although the remaining dextral strike-
ted by near pure dip-slip faulting along the	subduction zone, known as the Sunda megathrust, and nea
ada and the United States along the Cascadia	subduction zone, across more than 600 miles (966 km) fr
Seismicity cross-section, Kuril Islands	subduction zone, 15 November 2006, 8.3 Mw event marked
n Sea Plate, causing the Hellenic Trench and	subduction zone.
mic zone) is a deep active seismic area in a	subduction zone.
Trench and forms part of the Kermadec-Tonga	Subduction Zone.
meets the plate beneath northern Honshu in a	subduction zone.
ally look at it, the Puerto Rico trench is a	subduction zone: where the North American plate subduct
Some other	subduction zones have such earthquakes every 100 to 200
gneous rocks that are interpreted to form in	subduction zones from the mixing of mantle material wit
The andesite line parallels the	subduction zones and deep oceanic trenches around the P
It is a triple junction and three	subduction zones are involved.
The sinking of cold lithosphere at	subduction zones is another example of downwelling in p
oad, curving scarp resembles some of Earth's	subduction zones where crustal plates are pushed over e
In rocks in	subduction zones, that are transported to great depths
rocks typically are found in the arcs above	subduction zones, commonly in volcanic arcs, and partic
main places where partial melting occurs are	subduction zones, mid-ocean ridges and hotspots.
Around	subduction zones, various sources produce helium-3 in n
ds are unrelated to convergent boundaries or	subduction zones.
nd arcs and continental margins above active	subduction zones.

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