Title: |
PERMEABLE FRACTURES IN THE KAKKONDA GRANITE OF WELL WD-1B, JAPAN |
Authors: |
Osamu KATO, Yukihiro SAKAGAWA, Nobuo DOI, Kohei AKAKU, Yasukuni OHKUBO |
Key Words: |
Kakkonda, Japan |
Geo Location: |
Kakkonda, Japan; Sengan Geothermal Area |
Conference: |
Stanford Geothermal Workshop |
Year: |
1999 |
Session: |
GEOLOGY |
Language: |
English |
File Size: |
29KB |
View File: |
|
The Kakkonda Granite (Quaternary intrusion) has some feedpoints, which contribute to the steam production for the Kakkonda geothermal power plant. FMI (Schlumberger's Fullbore Formation MicroImager) log, resistivity log, gamma ray log, spinner log and temperature logs from NEDO*s well WD-1b have supplied information for determination of rock name and have revealed distributions of fractures. In the Kakkonda Granite, the fracture density analyzed from FMI log is far less than the other formations and the strike and dip of permeable fractures is partly different from that of the other formations.
Press the Back button in your browser, or search again.
Copyright 1999, Stanford Geothermal Program: Readers who download papers from this site should honor the copyright of the original authors and may not copy or distribute the work further without the permission of the original publisher.
Attend the nwxt Stanford Geothermal Workshop,
click here for details.