大地体
- 网络Geoid
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两层大地中三维体的激发极化与电阻率响应的积分方程模拟
Induced polarization and resistivity modeling of three-dimensional bodies in two-layered earth using integral equation
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郯&庐断裂两侧的地质差异由新太古代延续到早白垩世晚期,指示胶东半岛为一独立大地构造块体。
The geological contrasts on the two sides of the Tan-Lu Fault can be recognized from Neo-Archaean to Early Cretaceous , suggesting that the Shandong Peninsula is a separate tectonic block .