GSWA Trayning magnetic grid geodetic

Total magnetic intensity (TMI) data measures variations in the intensity of the Earth's magnetic field caused by the contrasting content of rock-forming minerals in the Earth crust. Magnetic anomalies can be either positive (field stronger than normal) or negative (field weaker) depending on the susceptibility of the rock. The data are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose.This GSWA Trayning magnetic grid geodetic has a cell size of 0.00035 degrees (approximately 36m). The units are in nanoTesla (or nT). The data used to produce this grid was acquired in 1997 by the WA Government, and consisted of 12657 line-kilometres of data at 150m line spacing and 50m terrain clearance.

总磁强度（Total Magnetic Intensity, TMI）数据用于测量由地壳内造岩矿物成分差异所引发的地球磁场强度变化。磁异常可分为正异常（磁场强度高于正常水平）与负异常（磁场强度低于正常水平），具体取决于岩石的磁化率。该数据集通过标准化流程进行处理，以确保所记录的响应仅源于地下岩石。经处理后得到的数据集可通过解译揭示地下地质构造。经处理的数据会由GA地球物理学家开展质量核查，以确保GA发布的最终数据符合使用需求。本GSWA Trayning磁测网格大地测量数据集的网格单元大小为0.00035度（约36米），数据单位为纳特斯拉（nanoTesla，简称nT）。用于生成该网格的数据由西澳大利亚政府于1997年采集，总测线长度达12657线公里，测线间距为150米，地形离地高度为50米。