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overloading of the Natal Thrust Front by the Natal Nappe Zone(passive) caused bya steepened normal geothermal gradient in the Mfongosi Group
Such a processledto the change in the geothermal gradient of the mantle wedge
by changes in the surface temperature that have modified the temperature of the rocks at these shallow depths(passive) are caused bychanges in the geothermal gradient
changes in the surface temperature that have modified the temperature of the rocks at these shallow depths(passive) are caused bychanges in the geothermal gradient
by the Dust Storm(passive) caused bythe Atmospheric Potential Gradient
by recent tectonic activity(passive) caused bythe high geothermal gradient
An increase in formation thermal conductivitywould also causea decrease in geothermal gradient
by subduction(passive) caused bythe low geothermal gradient
because the mantle transports heat primarily by convectionleadingto a geothermal gradient that is determined by the mantle adiabat
the circulation of terrestrial internal fluids(passive) is strongly influenced byThe geothermal gradient in turn
the energyresultingfrom the natural geothermal gradient
the reasonsetup a heat gradient
gravitycausinga thermal gradient in the troposphere
the centre of the column(passive) is caused byA radial thermal gradient
Rapid active uplift of these mountainshas ledto an elevated geothermal gradient on the eastern side
the pressure will increasecausingan increase in temperature by geothermal gradient
by the edge of the vast high - pressure system currently in the North Pacific(passive) caused bygradient winds
The sample length ... not too longto causethermal gradient
by the energy being deposited by the electrodes(passive) caused bythermal gradient
low and high pressure(passive) caused byGradient winds
to achieve excellent adhesion on different substrates(passive) were designedInterfacial gradient layers
A noveldesignedthermal gradient
A very fine - grained , low - grade metamorphic rockresultsfrom the metamorphism of shale
hereinabove can be discretely variedto resultin a stepwise gradient of porosity
by subduction(passive) caused bythe geothermal gradient
by changes in the surface temperature that have modified the temperature of the rocks at these shallow depths(passive) are causedthe geothermal gradient
a force on the bodysetsup a hydrostatic gradient
heat to the melting processcontributeheat to the melting process
to weak layers which can survive for weeks in the snow until an avalanche occurscan also leadto weak layers which can survive for weeks in the snow until an avalanche occurs
the surface coverage(passive) caused bythe surface coverage
in contact metamorphismresultedin contact metamorphism
in significant gas generationhas resultedin significant gas generation
Generation of a huge interconnected sub - glacial liquid freshwater system of streams and lakes(passive) is caused byGeneration of a huge interconnected sub - glacial liquid freshwater system of streams and lakes
_ _ _ _ _ _ _ _ _ _ _ _ meltingcan cause_ _ _ _ _ _ _ _ _ _ _ _ melting
regular temperature variations on the surface ( diurnal cycle , changing seasonscauseregular temperature variations on the surface ( diurnal cycle , changing seasons
thermal diffusion(passive) caused bythermal diffusion
from surface temperature variationsresultingfrom surface temperature variations
the shallow seismicitymay causethe shallow seismicity
different parts of the same object to expand with different amountscausesdifferent parts of the same object to expand with different amounts
up an energy flowsetsup an energy flow
maturation of these formationscausedmaturation of these formations
in mantleresultedin mantle
the top of the support to shrink toward the centre of the machine ( ~32 mm ) while the bottom remains stablecausesthe top of the support to shrink toward the centre of the machine ( ~32 mm ) while the bottom remains stable
the phase distribution in this sampleinfluencedthe phase distribution in this sample
Geothermal Geothermal heatcontributesGeothermal Geothermal heat
dynamic moisture transport(passive) caused bydynamic moisture transport
ATES systems(passive) caused byATES systems
to good warmingwill leadto good warming
to filopodia shortening , misorientation ( see also ) and reduced migration ( see alsoleadsto filopodia shortening , misorientation ( see also ) and reduced migration ( see also
the interface pressure distributionwill influencethe interface pressure distribution
pressurealso causespressure
to phase separation OR flux flow ( e.g. nucleation of phase - slip linesleadsto phase separation OR flux flow ( e.g. nucleation of phase - slip lines
Cracks(passive) caused byCracks
to good warmingaloft will leadto good warming
to decreased ventilationleadsto decreased ventilation
fuelcausesfuel
in high stressresultsin high stress
groundwater flow into the streamcausesgroundwater flow into the stream
groundwater flowcausesgroundwater flow
the rise of rock temperature(passive) caused bythe rise of rock temperature
in meltingresultingin melting
the heat interaction between the system and the surroundings(passive) is ... caused bythe heat interaction between the system and the surroundings
alsocould ... contributealso
of two colors and a transition between themis composedof two colors and a transition between them