Abstract
The analysis of the natural remanent magnetization (N.R.M.) of the Jurassic limestones from the Transdanubian Central Mountains (T.C.M's) (6 sites, 137 samples) resulted in the following palaeomagnetic pole position: ф = 54°, λ = 289° with α 95 = 11°. This result is explicable from two entirely different points of view as follows: 1. (1) The T.C.M's may always have formed part of stable Europe but rotated 73° counterclockwise about a vertical axis relative to it. 2. (2) The T.C.M's may have formed part of the African plate in the Adriatic region, shared the movements of Africa relative to stable Europe until when rotated to some degree counterclockwise about a vertical axis.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
