| 1. | The actual equipotential surface of the earth that corresponds to sea level is called the geoid .
相当海平面的地球实际等位面称为重力平面。 |
| 2. | For cartographical purposes heights are necessarily recorded above the geoid (sea-level) .
就制图的目的来说，所以需记录的高程是高出大地水准面（海平面）的高程。 |
| 3. | Determination of fuxin quasi - geoid without gravity data
无重力数据情况下阜新似大地水准面的确定 |
| 4. | Undulation of the geoid
大地水准面的起伏 |
| 5. | Determination of quasi - geoid in mainland china using geopotential model and gps leveling data
水准数据确定我国大陆似大地水准面 |
| 6. | Surface of the geoid
大地平均面 |
| 7. | Geoid tangent plane
大地体切面 |
| 8. | Problem of piecing together between china mainland - geoid and altimetry - derived geoid in china sea area
我国海域大地水准面与大陆大地水准面的拼接研究 |
| 9. | But the data of them are ample so it will be effective to dive geoid by them
而地形资料和岩石密度资料既充足又可靠，用它们来精化高原山区的大地水准面会获得良好的效果。 |
| 10. | Finally , the ocean geoid of china is worked out with about six months topex / poseidon data
最后用20个周期的topex / poseidon数据解算出了中国局部地区海洋大地水准面起伏。 |
