RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES3003, doi:10.2205/2020ES000712, 2020

Figure 2. Lithological column of the Kop-Takyl section (a). Legend: 1 – clay, 2 – calcareous clay, 3 – clay with thin sandy layers, 4 – carbonate nodules, 5 – carbonate layers, 6 – layer boundaries. Variations curves of the magnetic characteristics from the depth of the section H: natural remanent magnetization NRM (b), natural remanent magnetization NRM$_{20}$ after alternating field demagnetization 20 mT – (c), magnetic susceptibility ${\ae} (d)$, remanent coercitive force $Bcr$ (e), coercitive force $Bc$ – (f).

 
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.
 

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