Determination of NRM Vs Age for the Oceanic Crust

该项目的目的是确定体积和地壳自然剩磁磁化（NRM）随海洋地壳年龄的变化。将使用来自MAGSAT卫星的磁异常数据和来自北太平洋和北大西洋的海面测量数据。这项工作将有助于解决有关海洋地壳内残余磁化获取机制的不确定性。

The objective of the project is to determine the variation in the bulk and crustal natural remanenet magnetization (NRM) with respect to age of the oceanic crust. Magnetic anomaly data from MAGSAT satellite and sea-surface measurements from the North Pacific and North Atlantic will be used. The work will help resolve uncertainty concerning the mechanism of acquisition of remenent magnetization within the oceanic crust.