利用该方法对黄海某区的实际重力资料进了断层参数反演，并得到了很好的效果。
We inversed the fault parameters of the factual gravity data of Yellow sea with this method and got a good result.
重力变化可能是由该区地壳形变、地壳深部质量迁移和断层蠕动共同作用引起的。
The Variation of gravity field in this area may be caused by the crustal deformation or deep transference and fault creep.
褶积法是用已知理论子波从重力观测场中提取断层信息的一种滤波方法。
Convolution method is a filtering method used to extract fault information from observed gravity field by adopting known theoretical wavelet.
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