Time-variations of temperature within a mountain range are calculated by applying the relaxation technique to solving an equation of thermal conduction in the following two-dimensional mountain models. 1) A mountain range which is formed by a rapid erosion. 2) Mountain formation is caused by water erosion, the speed of which is very slow and constant. 3) A volcanic intrusion penetrated a flat plain. The results of the computations indicate that an L-type isotherm pattern would not be actually observed in geothermal measurements provided the geologically accepted age of mountains is true. It is possible to roughly estimate the age of a volcanic dome if it is younger than a few 104 years. Mt. Minakamiyama, a volcanic dome in the central area ...
The development of regional metamorphism in areas of thickened continental crust is investigated in ...
Detailed knowledge of the effects of temperature on the thermal conductivity (λ) of rocks is essenti...
Abstract: This paper demonstrates two-dimensional time-dependent finite-difference modelling of Hima...
Time-variations of temperature within a mountain range are calculated by applying the relaxation tec...
Terrestrial heat flow was measured at 6 localities in Hokkaido District. Of these 6 localities, 3 (A...
A subcrustal convection current having a linear dimension of a few thousand kilometers accounts for ...
On the assumption that hot magma intrudes suddenly in a spherical cavity in the earth's crust, the c...
Terrestrial heat flow was measured in 5 localities in Kyushu District. Of these 5 localities, one (T...
Determination of terrestrial heat flow in Japan has been attempted for the first time. Geothermal gr...
Since 1957, terrestrial heat flow has been determined at 39 places on the Japanese Islands by the Ea...
It has long been recognized that, over geologic time, some regions experience repeated episodes of m...
We have investigated whether low temperature thermochronological datasets can be used to constrain t...
AbstractLow-temperature thermochronology is a widely used tool for revealing denudation histories of...
Temperature vs distances profiles during geological time were calculated for a variety of realistica...
Thermochronometer data offers a powerful tool for quantifying a wide range of geologic processes, su...
The development of regional metamorphism in areas of thickened continental crust is investigated in ...
Detailed knowledge of the effects of temperature on the thermal conductivity (λ) of rocks is essenti...
Abstract: This paper demonstrates two-dimensional time-dependent finite-difference modelling of Hima...
Time-variations of temperature within a mountain range are calculated by applying the relaxation tec...
Terrestrial heat flow was measured at 6 localities in Hokkaido District. Of these 6 localities, 3 (A...
A subcrustal convection current having a linear dimension of a few thousand kilometers accounts for ...
On the assumption that hot magma intrudes suddenly in a spherical cavity in the earth's crust, the c...
Terrestrial heat flow was measured in 5 localities in Kyushu District. Of these 5 localities, one (T...
Determination of terrestrial heat flow in Japan has been attempted for the first time. Geothermal gr...
Since 1957, terrestrial heat flow has been determined at 39 places on the Japanese Islands by the Ea...
It has long been recognized that, over geologic time, some regions experience repeated episodes of m...
We have investigated whether low temperature thermochronological datasets can be used to constrain t...
AbstractLow-temperature thermochronology is a widely used tool for revealing denudation histories of...
Temperature vs distances profiles during geological time were calculated for a variety of realistica...
Thermochronometer data offers a powerful tool for quantifying a wide range of geologic processes, su...
The development of regional metamorphism in areas of thickened continental crust is investigated in ...
Detailed knowledge of the effects of temperature on the thermal conductivity (λ) of rocks is essenti...
Abstract: This paper demonstrates two-dimensional time-dependent finite-difference modelling of Hima...