Oroclinal bending in the Caledonides of western Ireland: a mid-Palaeozoic feature controlled by a pre-existing structural grain (Dataset)

Conall Mac Niocaill; Mark A Smethurst; Paul D Ryan;

1998 || Magnetics Information Consortium (MagIC)

Paleomagnetic, rock magnetic, or geomagnetic data found in the MagIC data repository from a paper titled: Conall Mac Niocaill, Mark A Smethurst, Paul D Ryan (1998). Oroclinal bending in the Caledonides of western Ireland: a mid-Palaeozoic feature controlled by a pre-existing structural grain. Tectonophysics 299 (1-3):31-47. doi:10.1016/s0040-1951(98)00197-8.

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Source http://dx.doi.org/10.7288/V4/MAGIC/15005
Source publisher Magnetics Information Consortium (MagIC)
DOI 10.7288/V4/MAGIC/15005
Authors
  • Conall Mac Niocaill
  • Mark A Smethurst
  • Paul D Ryan
Contributors
  • Magnetics Information Consortium (MagIC)
  • Distributor
References
  • Mac Niocaill, C., Smethurst, M. A., & Ryan, P. D. (1998). Oroclinal bending in the Caledonides of western Ireland: a mid-Palaeozoic feature controlled by a pre-existing structural grain. Tectonophysics, 299(1–3), 31–47. https://doi.org/10.1016/s0040-1951(98)00197-8
  • 10.1016/S0040-1951(98)00197-8
  • IsDocumentedBy
Citation Niocaill, C. M., Smethurst, M. A., & Ryan, P. D. (1998). Oroclinal bending in the Caledonides of western Ireland: a mid-Palaeozoic feature controlled by a pre-existing structural grain (Dataset) (Version 2) [Data set]. Tectonophysics. https://doi.org/10.7288/V4/MAGIC/15005