Gravity variation distribution in high negative value region is just consistent with the second shear strain's high value region of strain field obtained from GPS observation.
重力负值变化高值区的分布与GPS观测给出的应变场第二剪应变高值区一致。
According to the data of gravity field in Haljun Basin, the regional distribution of gravity anomaly is obtained.
根据哈喇峻地区区域重力数据资料，给出区域重力异常分布特征。
The results show that distribution of gravity stress is complex, and tectonic stress field exists in shallow layers of the earth crust.
结果表明，地壳浅层的岩土自重应力场分布复杂，并存在构造应力场。
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