Microwave paleointensities from dyke chilled margins: a way to obtain long-term variations in geodynamo intensity for the last three billion years (Dataset)

Henry C. Halls; Nick J. McArdle; Martin N. Gratton; Mimi J. Hill; John Shaw;

2004 || Magnetics Information Consortium (MagIC)

Paleomagnetic, rock magnetic, or geomagnetic data found in the MagIC data repository from a paper titled: Henry C. Halls, Nick J. McArdle, Martin N. Gratton, Mimi J. Hill, John Shaw (2004). Microwave paleointensities from dyke chilled margins: a way to obtain long-term variations in geodynamo intensity for the last three billion years. Physics of the Earth and Planetary Interiors 147 (2-3):183-195. doi:10.1016/j.pepi.2004.03.013.

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Source http://dx.doi.org/10.7288/V4/MAGIC/17432
Source publisher Magnetics Information Consortium (MagIC)
DOI 10.7288/V4/MAGIC/17432
Authors
  • Henry C. Halls
  • Nick J. McArdle
  • Martin N. Gratton
  • Mimi J. Hill
  • John Shaw
Contributors
  • Magnetics Information Consortium (MagIC)
  • Distributor
References
  • Halls, H. C., McArdle, N. J., Gratton, M. N., Hill, M. J., & Shaw, J. (2004). Microwave paleointensities from dyke chilled margins: a way to obtain long-term variations in geodynamo intensity for the last three billion years. Physics of the Earth and Planetary Interiors, 147(2–3), 183–195. https://doi.org/10.1016/j.pepi.2004.03.013
  • 10.1016/J.PEPI.2004.03.013
  • IsDocumentedBy
Citation Halls, H. C., McArdle, N. J., Gratton, M. N., Hill, M. J., & Shaw, J. (2004). Microwave paleointensities from dyke chilled margins: a way to obtain long-term variations in geodynamo intensity for the last three billion years (Dataset) (Version 3) [Data set]. Physics of the Earth and Planetary Interiors. https://doi.org/10.7288/V4/MAGIC/17432