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Titlebook: Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism; International Confer Danis Nurgaliev,Valery Shcherbakov,Simo

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Low-Temperature Magnetic Properties and Magnetic Mineralogy of the Ropruchey Sill (Russian Karelia)rvations, the studied rocks can be classified into two groups, granodiorites and gabbro-diorites, with different magnetic mineralogy. In granodiorites, the only magnetic mineral is stoichiometric magnetite characterized by a Verwey transition temperature of 120–121 K. In gabbro-diorites, the magneti
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Intrusions of the Kulumbe River Valley, NW Siberian Traps Province: Paleomagnetism, Magnetic Fabric usion showing the reverse magnetic polarity has the geochemical features similar to the ore-bearing Norilsk-type intrusions. Based on the study of the magnetic fabric of the intrusions, we suggest that they were fed from the magma-conducting Imangda-Letninskiy fault.
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Comparison of the Porosity Determination on the Whole Core and Petrophysical Samples high speed of measurement. At the end of the paper, conclusions were drawn about the applicability and expediency of using the nuclear magnetic resonance method using a whole core in core analysis programs and obtaining filtration-volumetric characteristics of rocks.
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Carboniferous of the Russian Platform: Paleomagnetic Dataomagnetic field of reversed polarity. Only in the rocks of the Visean stage a small zone of normal polarity is found. Widespread late Paleozoic remagnetization of the Carboniferous rocks of the Russian Platform is detected.
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