Paleomagnetism of the late CambrianCrepicephalus-Aphelaspis trilobite zone boundary in North America—divergent poles from isochronous strata (Dataset)

S GILLETT;

1982 || Magnetics Information Consortium (MagIC)

Paleomagnetic, rock magnetic, or geomagnetic data found in the MagIC data repository from a paper titled: S GILLETT (1982). Paleomagnetism of the late CambrianCrepicephalus-Aphelaspis trilobite zone boundary in North America—divergent poles from isochronous strata. Earth and Planetary Science Letters 58 (3):383-394. doi:10.1016/0012-821x(82)90087-5.

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Source http://dx.doi.org/10.7288/V4/MAGIC/18761
Source publisher Magnetics Information Consortium (MagIC)
DOI 10.7288/V4/MAGIC/18761
Authors
  • S GILLETT
Contributors
  • Magnetics Information Consortium (MagIC)
  • Distributor
References
  • GILLETT, S. (1982). Paleomagnetism of the late CambrianCrepicephalus-Aphelaspis trilobite zone boundary in North America—divergent poles from isochronous strata. Earth and Planetary Science Letters, 58(3), 383–394. https://doi.org/10.1016/0012-821x(82)90087-5
  • 10.1016/0012-821X(82)90087-5
  • IsDocumentedBy
Citation S GILLETT. (1982). Paleomagnetism of the late CambrianCrepicephalus-Aphelaspis trilobite zone boundary in North America—divergent poles from isochronous strata (Dataset) (Version 3) [Data set]. Earth and Planetary Science Letters. https://doi.org/10.7288/V4/MAGIC/18761