Leveling total‐field aeromagnetic data with measured horizontal gradients

Autor: J. Bradley Nelson
Rok vydání: 1994
Předmět:
Zdroj: GEOPHYSICS. 59:1166-1170
ISSN: 1942-2156
0016-8033
DOI: 10.1190/1.1443673
Popis: Temporal changes in the earth’s magnetic field occur in the frequency band of millihertz to a few Hertz. Amplitudes of variations above 0.1 Hz are usually much smaller than 1 nT, changes of 50–100 nT over periods of a few hours are not uncommon.
Databáze: OpenAIRE