Hysteresis characteristics of subaeral deposits in the Baikal region

Kazanskii A. Yu.; Matasova G. G.; Shchetnikov A. A.; Filinov I. A.; Chegis V. V.

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Hysteresis characteristics of subaeral deposits in the Baikal region

机译：百京地区沉积物滞后特征

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The results of rock magnetic studies in four subaeral cis-Baikalian sections of different ages and geneses are described in detail. The similarities and distinctions in the formation of the magnetic properties of the sediments are established based on the analysis of the magnetic hysteresis parameters. The mechanisms responsible for the dissimilarity of the magnetic characteristics of the rocks in the different sections are identified. The variations in the composition, concentration, and particle size of the grains of magnetic fraction as a function of climate, geomorphologic factors, and volcanism are demonstrated.

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《Izvestiya. Physics of the solid earth》 |2017年第5期|共12页
作者
Kazanskii A. Yu.; Matasova G. G.; Shchetnikov A. A.; Filinov I. A.; Chegis V. V.;
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作者单位

Moscow MV Lomonosov State Univ Fac Geol Moscow 119991 Russia;

Russian Acad Sci Trofimuk Inst Petr Geol &

Geophys Siberian Branch Novosibirsk 630090 Russia;

Russian Acad Sci Inst Earths Crust Siberian Branch Irkutsk 664033 Russia;

Russian Acad Sci Inst Earths Crust Siberian Branch Irkutsk 664033 Russia;

Moscow MV Lomonosov State Univ Fac Geol Moscow 119991 Russia;

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正文语种 eng
中图分类地球物理学;地质学;
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Hysteresis characteristics of subaeral deposits in the Baikal region

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