Abstract
The results of surveys conducted in the Akan region, Hokkaido, in fiscal 1988-1990 are compiled in this report. Conducted were a geological/alteration zone survey, geochemical survey, gravity prospecting, electromagnetic surveillance (simplified magnetotelluric method), electric prospecting (Schlumberger method), electric prospecting (mise-a-la-masse method), heat flow rate survey, test boring, geothermal water survey, environmental impact survey, and so forth. The surveys resulted in conclusions mentioned below. Fractures running NE-SW are dominant, and those closely related to prominent geothermal signs are found in the Akan Seibu fault group in the western part of the Akan region. The test boring results show that there are high-temperature zones of 292.1 degrees C, 194.9 degrees C, and 245.9 degrees C. Geothermal fluids were discharged by well N2-AK-7 at a rate of 4.7-4.8 t/h in steam and 0.3-0.4 t/h in neutral SO{sub 4}-HCO{sub 3} type geothermal water. High-temperature steam-dominated geothermal resources are expected to exist deep in the ground in this region, and the area where the Akan Seibu fault group is distributed may be named as a location containing promising geothermal resources. (NEDO)
Citation Formats
None.
Geothermal development promotion survey report. No. 26. Akan region; 1988-1991 chinetsu kaihatsu sokushin chosa hokokusho. No. 26 Akan chiiki.
Japan: N. p.,
1992.
Web.
None.
Geothermal development promotion survey report. No. 26. Akan region; 1988-1991 chinetsu kaihatsu sokushin chosa hokokusho. No. 26 Akan chiiki.
Japan.
None.
1992.
"Geothermal development promotion survey report. No. 26. Akan region; 1988-1991 chinetsu kaihatsu sokushin chosa hokokusho. No. 26 Akan chiiki."
Japan.
@misc{etde_20316282,
title = {Geothermal development promotion survey report. No. 26. Akan region; 1988-1991 chinetsu kaihatsu sokushin chosa hokokusho. No. 26 Akan chiiki}
author = {None}
abstractNote = {The results of surveys conducted in the Akan region, Hokkaido, in fiscal 1988-1990 are compiled in this report. Conducted were a geological/alteration zone survey, geochemical survey, gravity prospecting, electromagnetic surveillance (simplified magnetotelluric method), electric prospecting (Schlumberger method), electric prospecting (mise-a-la-masse method), heat flow rate survey, test boring, geothermal water survey, environmental impact survey, and so forth. The surveys resulted in conclusions mentioned below. Fractures running NE-SW are dominant, and those closely related to prominent geothermal signs are found in the Akan Seibu fault group in the western part of the Akan region. The test boring results show that there are high-temperature zones of 292.1 degrees C, 194.9 degrees C, and 245.9 degrees C. Geothermal fluids were discharged by well N2-AK-7 at a rate of 4.7-4.8 t/h in steam and 0.3-0.4 t/h in neutral SO{sub 4}-HCO{sub 3} type geothermal water. High-temperature steam-dominated geothermal resources are expected to exist deep in the ground in this region, and the area where the Akan Seibu fault group is distributed may be named as a location containing promising geothermal resources. (NEDO)}
place = {Japan}
year = {1992}
month = {Mar}
}
title = {Geothermal development promotion survey report. No. 26. Akan region; 1988-1991 chinetsu kaihatsu sokushin chosa hokokusho. No. 26 Akan chiiki}
author = {None}
abstractNote = {The results of surveys conducted in the Akan region, Hokkaido, in fiscal 1988-1990 are compiled in this report. Conducted were a geological/alteration zone survey, geochemical survey, gravity prospecting, electromagnetic surveillance (simplified magnetotelluric method), electric prospecting (Schlumberger method), electric prospecting (mise-a-la-masse method), heat flow rate survey, test boring, geothermal water survey, environmental impact survey, and so forth. The surveys resulted in conclusions mentioned below. Fractures running NE-SW are dominant, and those closely related to prominent geothermal signs are found in the Akan Seibu fault group in the western part of the Akan region. The test boring results show that there are high-temperature zones of 292.1 degrees C, 194.9 degrees C, and 245.9 degrees C. Geothermal fluids were discharged by well N2-AK-7 at a rate of 4.7-4.8 t/h in steam and 0.3-0.4 t/h in neutral SO{sub 4}-HCO{sub 3} type geothermal water. High-temperature steam-dominated geothermal resources are expected to exist deep in the ground in this region, and the area where the Akan Seibu fault group is distributed may be named as a location containing promising geothermal resources. (NEDO)}
place = {Japan}
year = {1992}
month = {Mar}
}