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the subduction of the Indian continent beneath Tibet(passive) caused bythe direction of mantle flow
the most powerful processcausingmantle plumes to flow
many dynamic factorsinfluencingmantle movement
by this energy(passive) caused bymantle movement
volcanic activity which is known to be occurring there(passive) caused bymantle movement
this plateinfluencesmantle flow
These convection currentscausesthe mantle to flow
an magnetic field which is one of the driving forcesis causesthe mantle to flow
by slab - retreat(passive) caused bymantle flow
one surprise ... apparently too lightto influencethe mantle flow
the shear stresscausingflow in the mantle
The weight of the icecausedmantle rock
the driving forcesis causesthe mantle to flow
Subduction brings down water and other crustal materialscausingmantle melting
of three layers namely the crust(passive) is composedMANTLE 3.Earth
The addition of enriched mantle type I ( EMI ) materials as well asmay have ledmantle heterogeneity
the thickness of the crustinfluencesmantle melting
an ophiolite assemblagecomposed mainlyof mantle tectonite
partial melting processes(passive) probably caused bymantle heterogeneity
various physical process of heat transport within the mantle(passive) are caused byMantle currents
crustal extensioncausesmantle upwelling
the process(passive) was caused byMantle convection
by silicate and carbonate melts(passive) caused bymantle metasomatism
At < 4 > , the ascending aqueous fluid lowers the solidus temperatureto causemantle melting
by silicate and carbonate(passive) caused bymantle metasomatism
by fault activity(passive) caused bymantle uplift
large enoughto influencemantle circulation
by the high temperature deformation(passive) caused bycasing mantle
Tidal heatingcan causeoutgassing from the mantle
Huanghua depression natural gases with CO2 content in excess of 15 %resultedfrom mantle degassing
Eclogitic diamonds formed from oceanic crust Eclogitic diamonds formed in Earth soriginatemantle
by heat transfer from Earth?s core(passive) caused byliquefied mantle
heat transfer from Earth?s core(passive) caused byliquefied mantle
Feature multi fuel stove with granite hearth and handpaintedmantle
of very hot , dense rock(passive) is composedmantle
by plate tectonics(passive) caused bymantle
of Iron and Magnesium silicates(passive) is composedMantle
white mantelpiece shelf custom fireplace mantel corbels rope molding crownpaintedmantle
by the gravitational pull of the sun and the two moons of Mars(passive) caused bymantle
by the gravitational pull of the sun and the two moons over Mars(passive) caused bymantle
to the uplift of the regioncontributesto the uplift of the region
surface topographycan influencesurface topography
in aluminum - depleted igneous rocksresultedin aluminum - depleted igneous rocks
extension from the shear stresses at the base of the overriding platecausesextension from the shear stresses at the base of the overriding plate
extension from the shear stressescausesextension from the shear stresses
seismic activity(passive) may be influenced byseismic activity
losses(passive) caused bylosses
hyperpycnal flows at searesultinghyperpycnal flows at sea
meltingcould causemelting
deformation(passive) caused bydeformation
plate motionscausesplate motions
surface exhumationinfluencedsurface exhumation
to substantial so - called " dynamic topographycan also leadto substantial so - called " dynamic topography
the graben formation(passive) caused bythe graben formation
large strain rates at the rift marginscan causelarge strain rates at the rift margins
the disturbance(passive) caused bythe disturbance
normal stress and tangential stressescausesnormal stress and tangential stresses
to the Indian plate subduction as far as the BNScontributesto the Indian plate subduction as far as the BNS
Hawaii - Emperor Seamount(passive) caused byHawaii - Emperor Seamount
to produce shielding gasis ... designedto produce shielding gas
Bend in Hawaii - Emperor Seamount(passive) caused byBend in Hawaii - Emperor Seamount
these plates to move relative tocausesthese plates to move relative to
hotter water to rise to the surface of the tankcauseshotter water to rise to the surface of the tank
the mass transport(passive) caused bythe mass transport
fabricated , and subsequently tested to reduce the intra - aneurysmal blood flowwas designedfabricated , and subsequently tested to reduce the intra - aneurysmal blood flow
fast separation of oil and grease even at high temperaturescausingfast separation of oil and grease even at high temperatures
from the upstream approach channelresultsfrom the upstream approach channel
much fluidcan causemuch fluid
the crustcausingthe crust
parasitic dragcausingparasitic drag
volcanismcausingvolcanism
a harmonic wave movement in surrounding tissueswill causea harmonic wave movement in surrounding tissues
waves of uplift and subsidencecauseswaves of uplift and subsidence
net PRC2-dependent H3K27me3 modificationcould ... influencenet PRC2-dependent H3K27me3 modification
the crust to down warp and swell into domescausingthe crust to down warp and swell into domes
narrow rift zones , such as the Afar Triple Junctionmay causenarrow rift zones , such as the Afar Triple Junction
upward flow of the partial melt due to decrease in its densitywould causeupward flow of the partial melt due to decrease in its density
from indigenous mantleoriginatedfrom indigenous mantle
to tectonic activity , such as volcanic eruptions and earthquakes , on the crustleadsto tectonic activity , such as volcanic eruptions and earthquakes , on the crust
upward high - pressure(passive) caused byupward high - pressure