plume volume flux along the Walvis Ridge-Rio Grande Rise

The plume volume flux along the Walvis Ridge strike is estimated through methods including inversion of gravity anomaly for crustal thickness, excess crustal thickness isolation, and integration of excess crustal thickness to estimate magma production volumes including the RGR.

沿沃尔维斯海岭（Walvis Ridge）走向的地幔柱体积通量，可通过以下多种方法进行估算：利用重力异常反演地壳厚度、分离提取地壳剩余厚度，以及对地壳剩余厚度进行积分以估算包含RGR在内的岩浆产量。