Paleomagnetic field intensity during cooling of the sudbury irruptive 1700 million years ago (Dataset)

E. J. Schwarz; D. T. A. Symons;

1970 || Magnetics Information Consortium (MagIC)

Paleomagnetic, rock magnetic, or geomagnetic data found in the MagIC data repository from a paper titled: E. J. Schwarz, D. T. A. Symons (1970). Paleomagnetic field intensity during cooling of the sudbury irruptive 1700 million years ago. Journal of Geophysical Research 75 (32):6631-6640. doi:10.1029/jb075i032p06631.

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Source http://dx.doi.org/10.7288/V4/MAGIC/18460
Source publisher Magnetics Information Consortium (MagIC)
DOI 10.7288/V4/MAGIC/18460
Authors
  • E. J. Schwarz
  • D. T. A. Symons
Contributors
  • Magnetics Information Consortium (MagIC)
  • Distributor
References
  • Schwarz, E. J., & Symons, D. T. A. (1970). Paleomagnetic field intensity during cooling of the sudbury irruptive 1700 million years ago. Journal of Geophysical Research, 75(32), 6631–6640. https://doi.org/10.1029/jb075i032p06631
  • 10.1029/JB075I032P06631
  • IsDocumentedBy
Citation E. J. Schwarz, & D. T. A. Symons. (1970). Paleomagnetic field intensity during cooling of the sudbury irruptive 1700 million years ago (Dataset) (Version 5) [Data set]. Journal of Geophysical Research. https://doi.org/10.7288/V4/MAGIC/18460