INDUCTIVE AND REMANENT MAGNETIZATION OF ROCKS OF ZARECHENSKAYA AND NIKOLSKAYA MAGNETIC ANOMALIES (EASTERN COAST OF OZ. BAIKAL)
The remanent magnetization, magnetic susceptibility and its anisotropy, as well as the Q factor of the samples of rocks, from the Zarechenskaya and Nikolskaya magnetic anomalies have been determined. These anomalies locate near the Selenginskaya depression on the eastern coast of Lake Baikal. Knowledge of the magnetic properties of rock massifs that are the sources of these anomalies is necessary to assess the magnetoelastic coefficients, which may be different for remanent and inductive magnetization. This, in turn, will make it possible to further increase the reliability of the interpretation of the results of tectomagnetic monitoring performed here.