Abstract
Cumulative data from a three year survey of the Kitayuzawa district of Otaki Village (Iburi, Hokkaido) are analyzed. The district is a well known hot spring area, where spring temperatures exceed 90/sup 0/C. The three-year study included geological, geochemical, and geophysical surveys; electrical, magnetic, and microearthquake studies; and a test well of 500 ..pi.. depth. The hot spas are associated with intrusive zones (dikes) near the Kitayuzawa-Osaru River. These zones can be detected by magnetic surveys. Studies of rock alteration indicated that positive thermal anomalies are associated with zeolite zones. Based on the geochemical and geophysical data, it is estimated that the thermal energy discharged in the Kitayuzawa district is about 14.4 Mcal/s. The waters of these springs are characterized as simple, vadose hot-water. A low-resistivity zone surrounds the springs and extends to the eastern sector of the district. Future studies of the area will include more numerous and deeper exploratory boreholes in the eastern sector. About 40 illustrations are provided, and 29 references are given.
Citation Formats
Hayakawa, F, Konoya, M, Yokoyama, H, Wake, T, and Kakiichi, K.
Report on the geothermal survey of the Kitayuzawa district of Otaki Village, Iburi Province, Hokkaido. Hokkaido Kitayuzawa chiikino chinetsu chosa.
Japan: N. p.,
1974.
Web.
Hayakawa, F, Konoya, M, Yokoyama, H, Wake, T, & Kakiichi, K.
Report on the geothermal survey of the Kitayuzawa district of Otaki Village, Iburi Province, Hokkaido. Hokkaido Kitayuzawa chiikino chinetsu chosa.
Japan.
Hayakawa, F, Konoya, M, Yokoyama, H, Wake, T, and Kakiichi, K.
1974.
"Report on the geothermal survey of the Kitayuzawa district of Otaki Village, Iburi Province, Hokkaido. Hokkaido Kitayuzawa chiikino chinetsu chosa."
Japan.
@misc{etde_6519931,
title = {Report on the geothermal survey of the Kitayuzawa district of Otaki Village, Iburi Province, Hokkaido. Hokkaido Kitayuzawa chiikino chinetsu chosa}
author = {Hayakawa, F, Konoya, M, Yokoyama, H, Wake, T, and Kakiichi, K}
abstractNote = {Cumulative data from a three year survey of the Kitayuzawa district of Otaki Village (Iburi, Hokkaido) are analyzed. The district is a well known hot spring area, where spring temperatures exceed 90/sup 0/C. The three-year study included geological, geochemical, and geophysical surveys; electrical, magnetic, and microearthquake studies; and a test well of 500 ..pi.. depth. The hot spas are associated with intrusive zones (dikes) near the Kitayuzawa-Osaru River. These zones can be detected by magnetic surveys. Studies of rock alteration indicated that positive thermal anomalies are associated with zeolite zones. Based on the geochemical and geophysical data, it is estimated that the thermal energy discharged in the Kitayuzawa district is about 14.4 Mcal/s. The waters of these springs are characterized as simple, vadose hot-water. A low-resistivity zone surrounds the springs and extends to the eastern sector of the district. Future studies of the area will include more numerous and deeper exploratory boreholes in the eastern sector. About 40 illustrations are provided, and 29 references are given.}
place = {Japan}
year = {1974}
month = {Jan}
}
title = {Report on the geothermal survey of the Kitayuzawa district of Otaki Village, Iburi Province, Hokkaido. Hokkaido Kitayuzawa chiikino chinetsu chosa}
author = {Hayakawa, F, Konoya, M, Yokoyama, H, Wake, T, and Kakiichi, K}
abstractNote = {Cumulative data from a three year survey of the Kitayuzawa district of Otaki Village (Iburi, Hokkaido) are analyzed. The district is a well known hot spring area, where spring temperatures exceed 90/sup 0/C. The three-year study included geological, geochemical, and geophysical surveys; electrical, magnetic, and microearthquake studies; and a test well of 500 ..pi.. depth. The hot spas are associated with intrusive zones (dikes) near the Kitayuzawa-Osaru River. These zones can be detected by magnetic surveys. Studies of rock alteration indicated that positive thermal anomalies are associated with zeolite zones. Based on the geochemical and geophysical data, it is estimated that the thermal energy discharged in the Kitayuzawa district is about 14.4 Mcal/s. The waters of these springs are characterized as simple, vadose hot-water. A low-resistivity zone surrounds the springs and extends to the eastern sector of the district. Future studies of the area will include more numerous and deeper exploratory boreholes in the eastern sector. About 40 illustrations are provided, and 29 references are given.}
place = {Japan}
year = {1974}
month = {Jan}
}