Fig. 10From: Possible correlation between the vertical component of lithospheric magnetic field and continental seismicityThe TESD (Two Equivalent Source Dipole) model. a Bz (solid line) and its y-gradient (dashed line, absolute value); b the distribution of the 2D Bz. The two black dots are the centers of the two ESD; c the TESD sketch. The altitude is not in scale; d the distribution of 2D gradientBack to article page