Multicomponent natural remanent magnetization of migmatites, Mórágy area, southwest Hungary

Research output: Contribution to journalArticle

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Abstract

Radiometrically dated granitoids of migmatitic origin from southwestern Hungary display multicomponent NRM. The direction of the component of high-temperature origin corresponds to a 280- to 300-m.y. magnetic pole in the Northern Eurasian framework. It is overprinted by haematite magnetization of low-temperature (

Original languageEnglish
Pages (from-to)102-112
Number of pages11
JournalEarth and Planetary Science Letters
Volume47
Issue number1
DOIs
Publication statusPublished - 1980

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Hungary
natural remanent magnetization
magnetization
hematite
Magnetization
magnetic poles
Poles
Display devices
Temperature
Direction compound
ferric oxide

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)
  • Geochemistry and Petrology
  • Geophysics

Cite this

Multicomponent natural remanent magnetization of migmatites, Mórágy area, southwest Hungary. / Márton, E.

In: Earth and Planetary Science Letters, Vol. 47, No. 1, 1980, p. 102-112.

Research output: Contribution to journalArticle

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