RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES3003, doi:10.2205/2020ES000712, 2020
Figure 6. Stereographic projections of the components of the ellipsoid of anisotropy of magnetic susceptibility (a), where $K_1$ is the maximum component, $K_2$ is the intermediate component, and $K_3$ is the minimum component of the magnetic susceptibility tensor. Lithological column (b). Dependence of the lineation $L$ (c), foliation $F$ (d) and the anisotropy degree $P' (e)$ on the depth of the section H.
Citation: Pilipenko O. V., E. V. Filina, Yu. V. Rostovtseva, Z. Novruzov (2020), Petromagnetism and paleomagnetism of the Tarkhanian sediments in Kop-Takyl section (the Kerch Peninsula), Russ. J. Earth Sci., 20, ES3003, doi:10.2205/2020ES000712.
Copyright 2020 by the Geophysical Center RAS.
Generated from LaTeX source by ELXfinal, v.2.0 software package.