The East Coast Magnetic Anomaly
The East Coast Magnetic Anomaly
复制标题
东海岸磁异常
作者：
L. E. Alsop;M. Talwani
本文首次提出了一种东海岸磁异常模型，该模型包含了观测到的基底特征——一个一直位于异常向陆侧翼下方的正常断层。东海岸磁异常与世界上许多地区被动大陆边缘的斜坡异常相似。因此，该模型可用于解释边坡异常。
A model is proposed for the East Coast Magnetic Anomaly that, for the first time, incorporates an observed basement feature—a normal fault that consistently lies below the landward flank of the anomaly. The East Coast Magnetic Anomaly is similar to slope anomalies found over passive continental margins in many parts of the world. Thus the proposed model can be used to interpret slope anomalies in general.