Abstract
An electromagnetic surveillance using the simplified MT (magnetotelluric) method was conducted to help clarify the geothermal structure in the western part of the Hakkoda area, Aomori Prefecture. The survey covered approximately 60 km{sup 2,} and involved 38 survey points, 3 magnetic field components, 2 electric field components, not less than 10 measuring frequencies in the range of 0.01-125 Hz, and a measuring time of not less than 2 hours. An analysis was performed, with data previously collected at 60 points added to the data collected at the said 38 points. As the result, the resistivity structure in this area was divided into 3 layers of high-low-high as described from the surface to the depth, and the middle layer was further divided into 3 layers of high-middle-low and the bottom layer into 2 layers of high-low. The result conformed though roughly to the result obtained by the electrical logging carried out in the structure boring. In the geothermal zone including the Sukayu hot spa in the southeastern part of this area and along the Jogakura valley, there exist a complicated resistivity structure attributable to geothermal activities and a number of discontinuous lines of resistivity running in the directions of WNW-ESE and
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Citation Formats
None.
Fiscal 1998 geothermal development promotion survey. Annex to on-the-ground survey report, geothermal development promotion survey (Part 2. Electromagnetic surveillance using simplified MT method - No. 30: Western part of Hakkoda area); 1989 nendo chinetsu kaihatsu sokushin chosa. Chinetsu kaihatsu sokushin chosa chijo chosa hokokusho futai shiryo (Denji tansa (MT kan'i ho) hokokusho - No.30 Hakkoda seibu chiiki - 2).
Japan: N. p.,
1991.
Web.
None.
Fiscal 1998 geothermal development promotion survey. Annex to on-the-ground survey report, geothermal development promotion survey (Part 2. Electromagnetic surveillance using simplified MT method - No. 30: Western part of Hakkoda area); 1989 nendo chinetsu kaihatsu sokushin chosa. Chinetsu kaihatsu sokushin chosa chijo chosa hokokusho futai shiryo (Denji tansa (MT kan'i ho) hokokusho - No.30 Hakkoda seibu chiiki - 2).
Japan.
None.
1991.
"Fiscal 1998 geothermal development promotion survey. Annex to on-the-ground survey report, geothermal development promotion survey (Part 2. Electromagnetic surveillance using simplified MT method - No. 30: Western part of Hakkoda area); 1989 nendo chinetsu kaihatsu sokushin chosa. Chinetsu kaihatsu sokushin chosa chijo chosa hokokusho futai shiryo (Denji tansa (MT kan'i ho) hokokusho - No.30 Hakkoda seibu chiiki - 2)."
Japan.
@misc{etde_20313506,
title = {Fiscal 1998 geothermal development promotion survey. Annex to on-the-ground survey report, geothermal development promotion survey (Part 2. Electromagnetic surveillance using simplified MT method - No. 30: Western part of Hakkoda area); 1989 nendo chinetsu kaihatsu sokushin chosa. Chinetsu kaihatsu sokushin chosa chijo chosa hokokusho futai shiryo (Denji tansa (MT kan'i ho) hokokusho - No.30 Hakkoda seibu chiiki - 2)}
author = {None}
abstractNote = {An electromagnetic surveillance using the simplified MT (magnetotelluric) method was conducted to help clarify the geothermal structure in the western part of the Hakkoda area, Aomori Prefecture. The survey covered approximately 60 km{sup 2,} and involved 38 survey points, 3 magnetic field components, 2 electric field components, not less than 10 measuring frequencies in the range of 0.01-125 Hz, and a measuring time of not less than 2 hours. An analysis was performed, with data previously collected at 60 points added to the data collected at the said 38 points. As the result, the resistivity structure in this area was divided into 3 layers of high-low-high as described from the surface to the depth, and the middle layer was further divided into 3 layers of high-middle-low and the bottom layer into 2 layers of high-low. The result conformed though roughly to the result obtained by the electrical logging carried out in the structure boring. In the geothermal zone including the Sukayu hot spa in the southeastern part of this area and along the Jogakura valley, there exist a complicated resistivity structure attributable to geothermal activities and a number of discontinuous lines of resistivity running in the directions of WNW-ESE and N-S. This enabled an inference that there is a deep-seated geothermal source between Odake and Akamizusawa extending eastward from the said geothermal zone. (NEDO)}
place = {Japan}
year = {1991}
month = {Jan}
}
title = {Fiscal 1998 geothermal development promotion survey. Annex to on-the-ground survey report, geothermal development promotion survey (Part 2. Electromagnetic surveillance using simplified MT method - No. 30: Western part of Hakkoda area); 1989 nendo chinetsu kaihatsu sokushin chosa. Chinetsu kaihatsu sokushin chosa chijo chosa hokokusho futai shiryo (Denji tansa (MT kan'i ho) hokokusho - No.30 Hakkoda seibu chiiki - 2)}
author = {None}
abstractNote = {An electromagnetic surveillance using the simplified MT (magnetotelluric) method was conducted to help clarify the geothermal structure in the western part of the Hakkoda area, Aomori Prefecture. The survey covered approximately 60 km{sup 2,} and involved 38 survey points, 3 magnetic field components, 2 electric field components, not less than 10 measuring frequencies in the range of 0.01-125 Hz, and a measuring time of not less than 2 hours. An analysis was performed, with data previously collected at 60 points added to the data collected at the said 38 points. As the result, the resistivity structure in this area was divided into 3 layers of high-low-high as described from the surface to the depth, and the middle layer was further divided into 3 layers of high-middle-low and the bottom layer into 2 layers of high-low. The result conformed though roughly to the result obtained by the electrical logging carried out in the structure boring. In the geothermal zone including the Sukayu hot spa in the southeastern part of this area and along the Jogakura valley, there exist a complicated resistivity structure attributable to geothermal activities and a number of discontinuous lines of resistivity running in the directions of WNW-ESE and N-S. This enabled an inference that there is a deep-seated geothermal source between Odake and Akamizusawa extending eastward from the said geothermal zone. (NEDO)}
place = {Japan}
year = {1991}
month = {Jan}
}