RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES6013, doi:10.2205/2020ES000710, 2020 Figure 2. Estimation of consistency of paleointensity (left) paleoinclination (right) data with GGP model: probabilities $p$ on grey scale for series of GGP models as function of mean intensities of quadrupole $g_2^0$ (along horizontal) and octupole $g_3^0$ (along vertical) terms given in $\mu$T. Colored bands correspond to $p$-values (see main text). Copyright 2020 by the Geophysical Center RAS. Generated from LaTeX source by ELXfinal, v.2.0 software package. |