geothermal gradient ... determined by tectonicsetting1.1.3.1 Geothermal gradient
the measured thermal conductivitydoes influencethe geothermal gradient
at 35 ° C km−1 ( 63 mW m−2 basal heat flux(passive) was setThe geothermal gradient
many other factors , such as lithology , petrophysical properties , formation water activity , and tectonic geological background(passive) can be influenced byThe geothermal gradient
a molten hot core(passive) caused bythe geothermal gradient
the same upward migration of warmer fluids that transports the methane(passive) is probably caused bygeothermal gradient
higherresultedfrom the geothermal gradient ( Hajto 2011a
The Zn - enriched coal seams of the western zone of the USCBmay resultfrom the raised geothermal gradient
In Figure 10.17 the dashed lines are isotherms – lines of equal temperature[1resultingfrom the geothermal gradient
a rate(passive) set bya rate
from either a change in the thermal conductivity of the strata or exhumation eventresultingfrom either a change in the thermal conductivity of the strata or exhumation event
the rise of rock temperature(passive) caused bythe rise of rock temperature
from the heat - exchange processresultingfrom the heat - exchange process
higher host - rock temperature(passive) triggered byhigher host - rock temperature
convection mixing of the fluids at different levels in the reservoirwill causeconvection mixing of the fluids at different levels in the reservoir
the work environment to be warmercausesthe work environment to be warmer
the melting rocks to form such very hot and melted materials in the earth mantlecausesthe melting rocks to form such very hot and melted materials in the earth mantle
basal melting(passive) caused bybasal melting
the CO2(l ... to expand more rapidly than seawatercausesthe CO2(l ... to expand more rapidly than seawater
the temperature to surpass the maximum temperature at which hydrates remain stablecausesthe temperature to surpass the maximum temperature at which hydrates remain stable