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
This data set was acquired with a ship-based Gravimeter, Magnetometer, and Echosounder during Robert D. Conrad expedition RC0807 conducted in 1964 (Chief Scientist: Dr. John Ewing). These data files a
This data set was acquired with a ship-based Echosounder Sonar, Magnetometer, and Gravimeter during Vema expedition V3614 conducted in 1980 (Chief Scientist: Dr. Robert Leyden). These data files are o
