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

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

Mar 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980e%26psl..47..102m&link_type=abstract

Earth and Planetary Science Letters, Volume 47, Issue 1, p. 102-112.

Computer Science

1

Scientific paper

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 (<300°C) origin, which has a direction similar to the CRM of granite aplites and bostonite. The overprint is probably of uppermost Jurassic/Lower Cretaceous age.

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