- 1. 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.
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- 2. 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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- 3. 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.
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- 4. 印支末期—燕山期又遭受了吴川—四会断裂带的左行走滑韧性剪切变形、变质作用。
- In last Indonian-Yenshan Stage, They also underwent left-slipping ductile Shear deformation and metamorphism along Wuchuan-Sihui fault belt.
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- 5. 印支末期—燕山期又遭受了吴川—四会断裂带的左行走滑韧性剪切变形、变质作用。
- In last Indonian-Yenshan Stage, They also underwent left-slipping ductile Shear deformation and metamorphism along Wuchuan-Sihui fault belt.
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