Fig. 6From: Geophysical characteristics of a fault system in the northern Central Range of Taiwan and its applications for geothermal energy explorationOrientations of the bed boundaries. From 720 to 1480 m MD, the dominant strike of the strata rotated from N60–80°E (subfig. (a)) to N40–60°E (subfig. (b) to (c)), and the dominant dip direction rotated from the SE to the NW (subfig. (c) to (d)) near the well bottomBack to article page