It is highly needed to develop an effective method to test the reliability of the 3-D stratified velocity structure of the earth’s crust and upper mantle obtained by using the seismic tomography (ST) and to make full...It is highly needed to develop an effective method to test the reliability of the 3-D stratified velocity structure of the earth’s crust and upper mantle obtained by using the seismic tomography (ST) and to make full use of the ST results. In this note, a new method named stratified gravity anomaly (SGA) is presented. It not only can provide the stratified gravity effect of different layers in the earth’s interior but also can be used to test the results of the seismic tomography. Here, the research is mainly concentrated展开更多
基金Project supported by the National Natural Science Foundation of China.
文摘It is highly needed to develop an effective method to test the reliability of the 3-D stratified velocity structure of the earth’s crust and upper mantle obtained by using the seismic tomography (ST) and to make full use of the ST results. In this note, a new method named stratified gravity anomaly (SGA) is presented. It not only can provide the stratified gravity effect of different layers in the earth’s interior but also can be used to test the results of the seismic tomography. Here, the research is mainly concentrated
