caa a22 4500 46910483X CHVBK 20180323133054.0 cr unu---uuuuu 170328e19920601xx s 000 0 eng 10.1007/BF01614128 doi (NATIONALLICENCE)springer-10.1007/BF01614128 Kapička A. Geophysical Institute, Czechosl. Acad. Sci., Prague aut The stability of isothermal and natural remanent magnetic polarization under elastic deformation of rocks [Elektronische Daten] [A. Kapička] Summary: With the decreasing magnitude of the initial remanent condition of rocks, their pressure demagnetization gradually changes to pressure remanent magnetic polarization under elastic deformation. In both cases the physical cause of these changes are the irreversible changes of the domain structure of ferrimagnetic minerals. Under directional pressure the natural remanent magnetic polarization is affected namely by the generation of a relatively little stable pressure remanent magnetic polarization. With regard to paleomagnetic research, the essential thing is that secondary magnetization combined with possible elastic deformations of rocks in the Earth's crust can be eliminated relatively easily by magnetic cleaning. Academia, Publishing House of the Czechoslorak Academy of Sciences, 1992 Studia Geophysica et Geodaetica Kluwer Academic Publishers 36/2(1992-06-01), 168-176 0039-3169 36:2<168 1992 36 11200 https://doi.org/10.1007/BF01614128 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/BF01614128 text/html Onlinezugriff via DOI NATIONALLICENCE 100 1- Kapička A. Geophysical Institute, Czechosl. Acad. Sci., Prague aut NATIONALLICENCE 773 0- Studia Geophysica et Geodaetica Kluwer Academic Publishers 36/2(1992-06-01), 168-176 0039-3169 36:2<168 1992 36 11200 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer