Fig. 2From: Geophysical characteristics of a fault system in the northern Central Range of Taiwan and its applications for geothermal energy explorationTemperature logs of the studied well section. The 34H, 51H, and 61H logs were surveyed in drilling mud 34, 51, and 61 h after the end of drilling. The 92D log was surveyed after the mud in the well was replaced by clean water and shut-in for 92 days. The drastic temperature changes in the 1334–1346 m MD and 1405–1410 m MD intervals could be related to the fault cores of Fault Zone 4Back to article page