In situ hydraulic tests in the active fault survey tunnel, Kamioka Mine, excavated through the active Mozumi-Sukenobu Fault zone and their hydrogeological significance

• Published in: The island arc Vol. 15; no. 4; pp. 537 - 545
• Main Authors: Nohara, Tsuyoshi, Tanaka, Hidemi, Watanabe, Kunio, Furukawa, Noboru, Takami, Akira
• Format: Journal Article
• Language: English
• Published: Melbourne, Australia Blackwell Publishing Asia 01.12.2006
• Subjects: active fault; Atotsugawa Fault system; discharged water; hydraulic test; Mozumi-Sukenobu Fault; tunnel
• ISSN: 1038-4871; 1440-1738
• DOI: 10.1111/j.1440-1738.2006.00548.x

The spatial hydrogeological and structural character of the active Mozumi‐Sukenobu Fault (MSF) was investigated along a survey tunnel excavated through the MSF in the Kamioka Mine, central Japan. Major groundwater conduits on both sides of the MSF are recognized. One is considered to be a subvertical conduit between the tunnel and the surface, and the other is estimated to be a major reservoir of old meteoric water alongside the MSF. Our studies indicate that part of the MSF is a sub‐vertical continuous barrier that obstructs younger meteoric water observed in the south‐eastern part of the Active Fault Survey Tunnel (AFST) and water recharge to the rock mass intersected by the north‐western part of the AFST. The MSF might be a continuous barrier resulting in the storage of a large quantity of older groundwater to the northwest. The observations and results of in situ hydraulic tests indicate that the major reservoir is not the fault breccia associated with the northeast–southwest trending faults of the MSF, but the zone in which blocks of fractured rocks occur beside high angle faults corresponding to X shears whose tectonic stress field coincides with the present regional stress field and antithetic Riedel shears of the MSF. The results from borehole investigations in the AFST indicate that secondary porosity is developed in the major reservoir due to the destruction of filling minerals and fracture development beside these shears. The increase in hydraulic conductivity is not directly related to increased density of fractures around the MSF. Development of secondary porosity could cause the increase in hydraulic conductivity around the MSF. Our results suggest that minor conduits of the fracture network are sporadically distributed in the sedimentary rocks around the MSF in the AFST.