结合该区已知的地质构造特征综合分析，重力负值带是早元古宙拗拉槽边界深断裂和构造—岩浆岩带的反映。
Considering the known synthetical studies on the characteristics of geological structures, the negative gravitational belt is considered to be a deep fracture or a tectonicmagmatic belts.
深部地质与地球物理资料显示区内两板块深部结合带位置可能与表层存在较大差异，更加深了板块边界划分研究的复杂程度。
Some subsurface geology and Geophysics data revealed the possible of large gap between the boundaries' location of surface and subsurface, made the issue much more complex.
该算法通过检测临界带特征矢量参数的距离变化确定初始分段边界，结合动态规划方法提高分段的准确性。
The initial segment is determined by detecting the distance changes of the critical feature parameter vector. With the dynamic programming method, the segmental accuracy is improved.
该算法通过检测临界带特征矢量参数的距离变化确定初始分段边界，结合动态规划方法提高分段的准确性。
The initial segment is determined by detecting the distance changes of the critical feature parameter vector. With the dynamic programming method, the segmental accuracy is improved.
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