The Neoproterozoic climatic paradox: Equatorial palaeolatitude for Marinoan glaciation near sea level in South Australia (Dataset)

Phillip W. Schmidt; George E. Williams;

1995 || Magnetics Information Consortium (MagIC)

Paleomagnetic, rock magnetic, or geomagnetic data found in the MagIC data repository from a paper titled: Phillip W. Schmidt, George E. Williams (1995). The Neoproterozoic climatic paradox: Equatorial palaeolatitude for Marinoan glaciation near sea level in South Australia. Earth and Planetary Science Letters 134 (1-2):107-124. doi:10.1016/0012-821x(95)00106-m.

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Source http://dx.doi.org/10.7288/V4/MAGIC/18955
Source publisher Magnetics Information Consortium (MagIC)
DOI 10.7288/V4/MAGIC/18955
Authors
  • Phillip W. Schmidt
  • George E. Williams
Contributors
  • Magnetics Information Consortium (MagIC)
  • Distributor
References
  • Schmidt, P. W., & Williams, G. E. (1995). The Neoproterozoic climatic paradox: Equatorial palaeolatitude for Marinoan glaciation near sea level in South Australia. Earth and Planetary Science Letters, 134(1–2), 107–124. https://doi.org/10.1016/0012-821x(95)00106-m
  • 10.1016/0012-821X(95)00106-M
  • IsDocumentedBy
Citation Schmidt, P. W., & Williams, G. E. (1995). The Neoproterozoic climatic paradox: Equatorial palaeolatitude for Marinoan glaciation near sea level in South Australia (Dataset) (Version 3) [Data set]. Earth and Planetary Science Letters. https://doi.org/10.7288/V4/MAGIC/18955