subduction oor Indonesies

subduction

/səbˈdʌkʃən/ naamwoord
en
the action of being pushed or drawn beneath another object.

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Subduksi

en
geological process at tectonic plate boundaries
The region where a plate descends is called a subduction zone.
Daerah tempat turunnya sebuah lempeng disebut zona subduksi.
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The region where a plate descends is called a subduction zone.
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Back-arc basins are geologic basins, submarine features associated with island arcs and subduction zones.
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Focal mechanisms for earthquakes near Bali are dominantly thrust sense on both the subduction interface and the system of thrust faults to the north.
Apa yang kita tabrak?WikiMatrix WikiMatrix
Indonesia is highly active in terms of seismicity and volcanic eruptions, with a subduction zone and many faults.
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The rate of subduction on these plates is estimated to be about 15 cm per year.
Tidak dengan#, # orang sekalipunWikiMatrix WikiMatrix
Metasomatism is thought to be particularly important in changing the composition of mantle peridotite below island arcs as water is driven out of ocean lithosphere during subduction.
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Subduction-zone stratovolcanoes, such as Mount St. Helens, Mount Etna and Mount Pinatubo, typically erupt with explosive force: the magma is too stiff to allow easy escape of volcanic gases.
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The 1949 Ambato earthquake initially followed an intersection of several northwest-southeast-trending faults in the Inter-Andean Valley which were created by the subduction of the Carnegie Ridge.
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Broadly speaking, the theory of plate tectonics says that earthquakes and volcanoes will occur in similar regions —in rifts, especially oceanic rifts; in earth’s crust, where magma rises from the mantle through fissures; and at subduction zones, where one plate plunges under another.
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However, Defant and Drummond recognized that when young oceanic crust (less than 25 million years old) is subducted, adakites are typically produced in the arc.
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Subduction volcanism is the biggest threat to people in terms of both the number of eruptions observed and their occurrence near populated areas.
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A characteristic feature of this plate boundary is the gradual change from normal subduction (on the southern margin) to a collisional regime (on the northern margin) which produces the Taiwan orogeny.
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The Kula Plate is an ancient tectonic plate that used to subduct under Alaska.
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Near the Nazca subduction zone the recorded history of interplate earthquakes spans 80 years.
Tidak, tak usah bayarWikiMatrix WikiMatrix
The earthquake was caused by a rupture of the subduction interface.
Aku ada permintaanWikiMatrix WikiMatrix
The movement of the Nazca Plate over several hotspots has created some volcanic islands as well as east-west running seamount chains that subduct under South America.
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Then, over a period of about 100 million years, subduction occurs on an enormous scale, completely recycling the crust.
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Subduction zones contain some of the world’s deepest trenches.
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In both cases the change in arc geochemistry can be related to the evolving architecture of that particular subduction zone.
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The major slip events on the subduction zone interface are typically of megathrust type.
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Earthquakes in Ecuador stem from two major interrelated tectonic areas: the subduction of the Nazca Plate under the South American Plate and the Andean Volcanic Belt.
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Despite being a type location for calc-alkalic and subduction volcanism, the Andean Volcanic Belt has a large range of volcano-tectonic settings, such as rift systems and extensional zones, transpressional faults, subduction of mid-ocean ridges and seamount chains apart from a large range on crustal thicknesses and magma ascent paths, and different amount of crustal assimilations.
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Most magmas derived in subduction zones come from the mantle above the subducting plate when hydrous fluids are released from minerals that break down in the metamorphosed basalt, rise into the mantle, and initiate partial melting.
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To the south of Taiwan, oceanic crust of the Eurasian Plate is subducting beneath the Philippine Sea Plate creating an island arc, the Luzon Arc.
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The Java trench was generated by the oblique subduction of the Indo-Australian Plate into the Sunda plate at a rate of 61mm/y (in the south) and 51mm/y (in the north).
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88 sinne gevind in 2 ms. Hulle kom uit baie bronne en word nie nagegaan nie.