Autor:	O. V. Gusev, S. S. Solov’eva, V. S. Vechfinskii
Rok vydání:	2008
Předmět:	Basalt Magnetization Igneous rock Magnetic minerals General Earth and Planetary Sciences Barkhausen stability criterion Geophysics Geology Physics::Geophysics General Environmental Science Magnetic field
Zdroj:	Izvestiya, Physics of the Solid Earth. 44:256-259
ISSN:	1555-6506 1069-3513
DOI:	10.1134/s1069351308030099
Popis:	Igneous rocks are shown to possess a magnetic fabric that admits the occurrence of giant Barkhausen jumps. It is also demonstrated that magnetic minerals of rocks can preserve information on a few magnetic fields (differing even in origin) and a few thermal magnetization temperatures.
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_________::4e544aebd5a45c13391ad4dba59a3e24 https://doi.org/10.1134/s1069351308030099 Zobrazit plný text záznamu Full text from SpringerLink