The Sankeng geothermal field is located on the northeastern side of the Wuchuan Sihui deep fault and in the Sankeng synclinal karstic basin.
广东三坑地热田位于吴川—四会深大断裂带的东北侧，三坑向斜岩溶盆地内。
The western tongue has a synclinal bottom configuration, the axis of which plunges at a low angle towards the fault.
（结晶学）有三个以倾斜的角度交叉的不同晶轴。
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