Unfortunately this page does not have a mobile or narrow screen view. Please switch to a desktop computer or increase the size of your browser. For tablets try flipping the screen.
Data Publication
Paleomagnetic field intensity during cooling of the sudbury irruptive 1700 million years ago (Dataset)
E. J. Schwarz | D. T. A. Symons
Magnetics Information Consortium (MagIC)
(2014)
Paleomagnetic, rock magnetic, or geomagnetic data found in the MagIC data repository from a paper titled: Paleomagnetic field intensity during cooling of the sudbury irruptive 1700 million years ago
Keywords
Originally assigned keywords
Source publisher
Magnetics Information Consortium (MagIC)
DOI
10.7288/V4/MAGIC/18460
Authors
E. J. Schwarz
D. T. A. Symons
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
IsCitedBy
E. J. Schwarz, & D. T. A. Symons. (2014). <i>Paleomagnetic field intensity during cooling of the sudbury irruptive 1700 million years ago (Dataset)</i> (Version 4) [Data set]. Magnetics Information Consortium (MagIC). https://doi.org/10.7288/V4/MAGIC/15545
10.7288/V4/MAGIC/15545
IsNewVersionOf
Citiation
E. J. Schwarz, & D. T. A. Symons. (2014). Paleomagnetic field intensity during cooling of the sudbury irruptive 1700 million years ago (Dataset) (Version 5) [Data set]. Magnetics Information Consortium (MagIC). https://doi.org/10.7288/V4/MAGIC/18460