Geochemical constraints on the origin of secondary magnetizations in the Cambro-Ordovician Royer Dolomite, Arbuckle Mountains, southern Oklahoma (Dataset)

R.D. Elmore; K. Cates; G. Gao; L. Land;

1994 || Magnetics Information Consortium (MagIC)

Paleomagnetic, rock magnetic, or geomagnetic data found in the MagIC data repository from a paper titled: R.D. Elmore, K. Cates, G. Gao, L. Land (1994). Geochemical constraints on the origin of secondary magnetizations in the Cambro-Ordovician Royer Dolomite, Arbuckle Mountains, southern Oklahoma. Physics of the Earth and Planetary Interiors 85 (1-2):3-13. doi:10.1016/0031-9201(94)90004-3.

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Source http://dx.doi.org/10.7288/V4/MAGIC/13521
Source publisher Magnetics Information Consortium (MagIC)
DOI 10.7288/V4/MAGIC/13521
Authors
  • R.D. Elmore
  • K. Cates
  • G. Gao
  • L. Land
Contributors
  • Magnetics Information Consortium (MagIC)
  • Distributor
References
  • Elmore, R. D., Cates, K., Gao, G., & Land, L. (1994). Geochemical constraints on the origin of secondary magnetizations in the Cambro-Ordovician Royer Dolomite, Arbuckle Mountains, southern Oklahoma. Physics of the Earth and Planetary Interiors, 85(1–2), 3–13. https://doi.org/10.1016/0031-9201(94)90004-3
  • 10.1016/0031-9201(94)90004-3
  • IsDocumentedBy
Citation R.D. Elmore, K. Cates, G. Gao, & L. Land. (1994). Geochemical constraints on the origin of secondary magnetizations in the Cambro-Ordovician Royer Dolomite, Arbuckle Mountains, southern Oklahoma (Dataset) (Version 2) [Data set]. Physics of the Earth and Planetary Interiors. https://doi.org/10.7288/V4/MAGIC/13521