The complex NRM of the Permocarboniferous Bademli Redbeds
Abstract
The analysis of the NRM of 27 Permocarboniferous samples from a nappe in the Tauride Chains revealed that in most samples three magnetic components were present. Two of the components are thought to be secondary due to remagnetization in Early Tertiary, and Recent times. The third and hardest component is assumed to be Permocarboniferous. It yielded an anomalous paleomagnetic direction, though the low inclination value indicates an equatorial position during the Permocarboniferous.
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