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A new method for the determination of paleointensity from the A.R.M. properties of rocksThe relation between the mechanisms of thermoremanent magnetization (TRM) and anhysteretic remanent magnetization (ARM) considered by Nagata (1961) is utilized in the new method. It is shown experimentally that the ratio of room temperature TRM and ARM susceptibilities can be determined quantitatively from the intrinsic magnetic parameters of the rock. Questions of the theoretical background of the method are examined along with details regarding the experimental technique.-
Document ID
19750026357
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
External Source(s)
doi:10.1016/0012-821X(74)90190-3
Authors
Banerjee, S. K.
Mellema, J. P. (Minnesota, University Minneapolis, Minn., United States)
Date Acquired
August 8, 2013
Publication Date
September 1, 1974
Publication Information
Publication: Earth and Planetary Science Letters
Volume: 23
Issue: 2, Se
Subject Category
Geophysics
Accession Number
75A10429
Funding Number(s)
CONTRACT_GRANT: NGR-24-005-248
CONTRACT_GRANT: NSF GA-31299
Distribution Limits
Public
Copyright
Other

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