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Takigami geothermal system, northeastern Kyushu, Japan
Abstract The Takigami geothermal reservoir is bound
The Takigami geothermal reservoir is bounded by a system of faults and fractures oriented along two main directions, north to south and east to west. The Noine fault has a large vertical displacement and trends north to south, dividing the subsurface characteristics of resistivity, permeability, temperature and reservoir depth. The Takigami geothermal fluid has a near neutral pH and is of the Na–Cl type, with a chloride content ranging from 400 to 600 ppm. The southwestern part of the area has the highest subsurface temperature, up to 250°C. The deep fluid originates from the southwest, and flow is mainly to the north and partly to the east along faults and fractures, decreasing in temperature with increasing lateral flow.
temperature with increasing lateral flow.  +
Author Shigetsugu Furuyaa  + , Michio Aokia  + , Hiroki Gotoha  + , Teruo Takenakab  +
Citation Shigetsugu Furuyaa, Michio Aokia, Hiroki Gotoha, Teruo Takenakab. 04/2000. [[Takigami geothermal system, northeastern Kyushu, Japan]]. Geothermics. 29(2):191-211.  +
DOI Takigami geothermal system, northeastern Kyushu, Japan  +
Document type Journal Article  +
Foaf/Page http://www.sciencedirect.com/science/article/pii/S0375650599000590  +
Link http://www.sciencedirect.com/science/article/pii/S0375650599000590  +
Name Takigami geothermal system, northeastern Kyushu, Japan  +
PublicationDate April 2000  +
Publisher Geothermics  +
ReferenceGenre Geothermal  +
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Takigami geothermal system, northeastern Kyushu, Japan + , Takigami geothermal system, northeastern Kyushu, Japan +
Categories References , Geothermal References
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22:23:30, 21 April 2015  +
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Takigami Geothermal Area + ReferenceForReservoirTemp
 
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