residual gravity anomaly

基本解釋

In dealing with the gravity data of some basin, obtain the residual gravity anomaly applying finite element method.
在某盆地的重力資料處理中，用有限元插值法分離出該區(qū)的局部重力異常。
The residual gravity anomaly was mainly produced by rolling basement of the basin and the regional gravity anomaly by the Moho rolling.
推斷引起剩余重力異常的主要原因是盆地基底的起伏，引起區(qū)域重力異常的主要原因是莫霍面起伏。
However, there occurs 5-70 milligals gravity anomaly in this region, the residual anomaly being 30-50 milligals after eliminating the effect of Mohorovicic discontinuity.
然而，在此區(qū)卻出現(xiàn)了5—70毫伽的重力異常值，從中去除莫氏界面的影響，其剩余異常值還有30—50毫伽。