Paleomagnetism of baked sedimentary rocks in the Newark and Culpeper basins: Evidence for the J1 cusp and significant Late Triassic apparent polar wander from the Mesozoic basins of North America (Dataset)

Kenneth P. Kodama; Maria T. Cioppa; Elizabeth Sherwood; Andrew C. Warnock;

1994 || Magnetics Information Consortium (MagIC)

Paleomagnetic, rock magnetic, or geomagnetic data found in the MagIC data repository from a paper titled: Kenneth P. Kodama, Maria T. Cioppa, Elizabeth Sherwood, Andrew C. Warnock (1994). Paleomagnetism of baked sedimentary rocks in the Newark and Culpeper basins: Evidence for the J1 cusp and significant Late Triassic apparent polar wander from the Mesozoic basins of North America. Tectonics 13 (4):917-928. doi:10.1029/94tc00294.

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Source http://dx.doi.org/10.7288/V4/MAGIC/16070
Source publisher Magnetics Information Consortium (MagIC)
DOI 10.7288/V4/MAGIC/16070
Authors
  • Kenneth P. Kodama
  • Maria T. Cioppa
  • Elizabeth Sherwood
  • Andrew C. Warnock
Contributors
  • Magnetics Information Consortium (MagIC)
  • Distributor
References
  • Kodama, K. P., Cioppa, M. T., Sherwood, E., & Warnock, A. C. (1994). Paleomagnetism of baked sedimentary rocks in the Newark and Culpeper basins: Evidence for the J1 cusp and significant Late Triassic apparent polar wander from the Mesozoic basins of North America. Tectonics, 13(4), 917–928. Portico. https://doi.org/10.1029/94tc00294
  • 10.1029/94TC00294
  • IsDocumentedBy
Citation Kodama, K. P., Cioppa, M. T., Sherwood, E., & Warnock, A. C. (1994). Paleomagnetism of baked sedimentary rocks in the Newark and Culpeper basins: Evidence for the J1 cusp and significant Late Triassic apparent polar wander from the Mesozoic basins of North America (Dataset) (Version 2) [Data set]. Tectonics. https://doi.org/10.7288/V4/MAGIC/16070