III. The origin of the palaeomagnetism of the Torridonian sandstones of North-West Scotland

• IRVING E.

抄録

The ferromagnetic minerals occurring in the Torridonian sandstones are described. Detrital grains of specularite often containing small inclusions of magnetite are present; the red haematitic cement is shown to be ferromagnetic. Possible origins of the natural remanent magnetization are discussed, and it is concluded that the evidence, especially the correlation of dispersion of the n.r.m. directions with the grain size of specimens, favours a depositional type of magnetization.

収録刊行物

• Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences

  Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences 250 (974), 100-110, 1957-08-29

  The Royal Society

詳細情報

• CRID: 1361137046141941760
• NII論文ID: 30035332040
• NII書誌ID: AA00772891
• DOI: 10.1098/rsta.1957.0014
• ISSN: 20540272
• ISSN: 00804614
• Web Site: https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.1957.0014
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