Our proposal was supported by terrestrial heat flow data, Bougueranomaly inversion and neotectonic studies.
拆沉失稳机制得到了大地热流、布格重力异常反演和新构造运动研究结果的支持。
2
By using 3-d gravity forward calculation, we obtained the deep gravity anomalies of Tai-wan from its Bougueranomaly. Its depth corresponds to the lower crust.
经过三维重力正演计算，我们从台湾的布格重力异常中求得了深部重力异常，其深度相当于地壳下层。
3
The gravity data processing includes displacement rectification, normal field correction, Eotvos rectification, Bouguer correction and Grany anomaly correction.