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Table 1 Results on Paleointensity measurements of plagioclase samples

From: Paleomagnetic studies on single crystals separated from the middle Cretaceous Iritono granite

Sample ID NRM0 (pAm2) HL (mT) f MAD (°) ARM0 (pAm2) NRM–TRM1* TRM1–TRM2*
     Slope R Slope R F (μT)
Successful samples           
 9004 134.6 0 1.000 9.2 248.7 0.945 ± 0.064 0.9647 1.054 ± 0.050 0.9827 47.2 ± 3.2
 9009 93.0 40 0.700 9.8 147.2 1.142 ± 0.100 0.9706 1.094 ± 0.021 0.9972 57.1 ± 5.0
 9020 484.0 45 0.486 9.2 616.5 1.253 ± 0.083 0.9658 1.048 ± 0.026 0.9944 62.6 ± 4.2
 9036 344.0 45 0.499 10.2 794.1 0.862 ± 0.120 0.9075 1.082 ± 0.021 0.9966 43.1 ± 6.0
 9099 193.1 0 1.000 11.0 319.0 1.558 ± 0.126 0.9456 1.051 ± 0.056 0.9744 77.9 ± 6.3
 9054 264.8 35 0.570 15.9 355.1 1.457 ± 0.187 0.9075 1.078 ± 0.061 0.9710 72.8 ± 9.4
 9070 126.7 15 0.942 12.9 336.0 0.974 ± 0.096 0.9259 0.968 ± 0.032 0.9900 48.7 ± 4.8
 34,019 104.0 20 0.868 11.0 265.5 1.129 ± 0.106 0.9394 0.960 ± 0.031 0.9908 56.4 ± 5.3
 44,092 64.7 10 0.992 10.6 117.1 1.007 ± 0.096 0.9301 1.008 ± 0.041 0.9851 50.3 ± 4.8
          Mean 57.4 ± 11.8
Failed samples
 9013 90.8 35 0.677 7.9 106.9 1.424 ± 0.095 0.9785 0.887 ± 0.051 0.9728 71.2 ± 4.7
 9016 79.5 35 0.600 11.1 156.0 0.714 ± 0.058 0.9714 1.297 ± 0.065 0.9805 35.7 ± 2.9
 9035 269.6 No primary magnetization 552.5 0.961 ± 0.035 0.9872  
 9047 181.6 Low linearity in NRM/TRM1* plot 392.7   0.971 ± 0.029 0.9909  
 9061 174.4 20 0.860 8.9 335.7 0.935 ± 0.086 0.9420 1.232 ± 0.070 0.9705 46.7 ± 4.3
 9113 495.7 25 0.855 8.9 624.4 1.611 ± 0.111 0.9662 1.173 ± 0.065 0.9722 80.6 ± 5.6
 44,106 88.5 20 0.923 5.9 120.5 1.216 ± 0.104 0.9465 0.849 ± 0.078 0.9276 60.8 ± 5.2
 44,108 76.2 0 1.000 5.3 132.4 1.310 ± 0.062 0.9847 0.627 ± 0.119 0.7706 65.5 ± 3.1
  1. NRM0 NRM intensity before LTD, HL the lowest AFD step used in paleointensity estimate, f NRM fraction of the primary magnetization used in paleointensity estimate, ARM0 intensity of ARM0 before LTD, R correlation coefficient, F estimated paleointensity