Abstract
The results of surveys conducted in the Hishikari region, Kagoshima Prefecture, in fiscal 1987-1989 are compiled in this report. Conducted were a geological/alteration zone survey, geochemical survey, electric prospecting, electromagnetic surveillance, gravity prospecting, heat flow rate survey, test boring, environmental impact survey, and so forth. The surveys resulted in conclusions mentioned below. According to the underground temperature distribution based on the results of the heat flow rate survey, test boring, and so forth, temperature is low at the western part of the Hishikari region where there is a low gravity anomaly and high in the zone in the ENE-WSW direction where there is a high gravity anomaly. The present ground temperature is lower than the fluid inclusion homogenization temperature by approximately 120-140 degrees C. It is deduced that the geothermal water reservoir lies in the Quatenary volcanic rocks or in a fracture zone that develops in the Shimanto supergroup. It is inferred that the geothermal water producing the hot spring water all originates in meteoric water staying long in the ground. It is also inferred that volcanic gas or the like contributes but a little to the formation of the geothermal system but that the contribution is great of the
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Citation Formats
None.
Geothermal development promotion survey report. No. 25. Hishikari region; 1987-1989 chinetsu kaihatsu sokushin chosa hokokusho. No. 22 Hishikari chiiki.
Japan: N. p.,
1990.
Web.
None.
Geothermal development promotion survey report. No. 25. Hishikari region; 1987-1989 chinetsu kaihatsu sokushin chosa hokokusho. No. 22 Hishikari chiiki.
Japan.
None.
1990.
"Geothermal development promotion survey report. No. 25. Hishikari region; 1987-1989 chinetsu kaihatsu sokushin chosa hokokusho. No. 22 Hishikari chiiki."
Japan.
@misc{etde_20316281,
title = {Geothermal development promotion survey report. No. 25. Hishikari region; 1987-1989 chinetsu kaihatsu sokushin chosa hokokusho. No. 22 Hishikari chiiki}
author = {None}
abstractNote = {The results of surveys conducted in the Hishikari region, Kagoshima Prefecture, in fiscal 1987-1989 are compiled in this report. Conducted were a geological/alteration zone survey, geochemical survey, electric prospecting, electromagnetic surveillance, gravity prospecting, heat flow rate survey, test boring, environmental impact survey, and so forth. The surveys resulted in conclusions mentioned below. According to the underground temperature distribution based on the results of the heat flow rate survey, test boring, and so forth, temperature is low at the western part of the Hishikari region where there is a low gravity anomaly and high in the zone in the ENE-WSW direction where there is a high gravity anomaly. The present ground temperature is lower than the fluid inclusion homogenization temperature by approximately 120-140 degrees C. It is deduced that the geothermal water reservoir lies in the Quatenary volcanic rocks or in a fracture zone that develops in the Shimanto supergroup. It is inferred that the geothermal water producing the hot spring water all originates in meteoric water staying long in the ground. It is also inferred that volcanic gas or the like contributes but a little to the formation of the geothermal system but that the contribution is great of the heat supplied from the magma pool. (NEDO)}
place = {Japan}
year = {1990}
month = {Mar}
}
title = {Geothermal development promotion survey report. No. 25. Hishikari region; 1987-1989 chinetsu kaihatsu sokushin chosa hokokusho. No. 22 Hishikari chiiki}
author = {None}
abstractNote = {The results of surveys conducted in the Hishikari region, Kagoshima Prefecture, in fiscal 1987-1989 are compiled in this report. Conducted were a geological/alteration zone survey, geochemical survey, electric prospecting, electromagnetic surveillance, gravity prospecting, heat flow rate survey, test boring, environmental impact survey, and so forth. The surveys resulted in conclusions mentioned below. According to the underground temperature distribution based on the results of the heat flow rate survey, test boring, and so forth, temperature is low at the western part of the Hishikari region where there is a low gravity anomaly and high in the zone in the ENE-WSW direction where there is a high gravity anomaly. The present ground temperature is lower than the fluid inclusion homogenization temperature by approximately 120-140 degrees C. It is deduced that the geothermal water reservoir lies in the Quatenary volcanic rocks or in a fracture zone that develops in the Shimanto supergroup. It is inferred that the geothermal water producing the hot spring water all originates in meteoric water staying long in the ground. It is also inferred that volcanic gas or the like contributes but a little to the formation of the geothermal system but that the contribution is great of the heat supplied from the magma pool. (NEDO)}
place = {Japan}
year = {1990}
month = {Mar}
}