研究表明，吴川四会断裂带是一条切壳深断裂。
The research indicates that the Wuchuan Sihui fault is a crust cutting deep fault.
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 Sankeng geothermal field is located on the northeastern side of the Wuchuan Sihui deep fault and in the Sankeng synclinal karstic basin.
这些洞穴的大致走向都沿NNE向，这是受四会—吴川深断裂带的影响而造成的。
The strikes of the caves are almost along the NNEdirection because of the influence of Sihui—Wuchuan deep fault belt.
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