RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 7, ES3003, doi:10.2205/2005ES000175, 2005

2005ES000175-fig06.html
Figure 6. Transitional Lower Jaramillo zone (Adjidere section, West Turkmenia). (A) Matuyama chronozone, (B) reflection of the inversion triggering mechanism or of the early reversal stage; (C) reflection of the reversal, (D) Jaramillo chronozone. Declination and inclination are given in the stratigraphic system of the coordinates, each depth level is characterized by the average value for five specimens after their complete thermal demagnetization and component analyses. The relative paleointensity Rns=(NRM300o-NRM500o/IRM300o-IRM500o) times 1000, IRM in the field of 0.9 T.

RJES

Citation: Gurarii, G. Z. (2005), Geomagnetic field reversals: Main results and basic problems, Russ. J. Earth Sci., 7, ES3003, doi:10.2205/2005ES000175.

Copyright 2005 by the Russian Journal of Earth Sciences
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