Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province.
断裂带控制了福建生代壳变今壳运动的南北差异。
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The same is true of cracks and other deformations in the Earth's crust, which can sometimes be traced across plates.
地壳缝和其他变形是如此,有时可板块追踪。
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