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Therefore, the paleomagnetic mean direction of IWT was excluded in further tectonic discussion.
In Fig. 5c, we plot the mean direction of ThD and AFD experiments.
The mean direction of the two specimens from the same horizon was used for the calculation if both survived.
The actual sediment-transport directions during normal conditions are shown as the mean direction of tracer results (see Fig. 4a).
The boxes show the mean direction of the observed (θmax and θmin) and modeled stress indicators (θmaxmodel and θminmodel) and the difference between the observed and modeled orientations.
The mean direction of these seven hematite-bearing samples is consistent with that of twelve other magnetite-bearing samples from the same sampling site in 95% confidence limits.
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The laminate cross-sections are made along and perpendicular to the mean directions of the impregnated fibre bundles (yarns).
When combined, the paleomagnetic site mean direction and paleopole for the entire A4 are D/I = 10.9°/50.1° (α 95 = 5.6°, k = 38.6) and VGP = 79.8°N/242.4°E (A 95 = 5.0°, N = 18) (Table 2). Figure 9 Paleomagnetic site mean directions of A4 pass the reversal test.
As illustrated in Figure 9, the mean directions of propagation point systematically, but not statistically significantly, to areas more frontal than the head vertex.
Of these, 19 show α 95 values of less than 16°, yielding a more eastward-deflected formation-mean direction of D = 49.9° (ΔD = 9.5°), I = 51.9°, α 95=5.8°8°.
Reliable site-mean directions for 19 sites yield a tilt-corrected formation-mean direction of D = 10.5°, I = 41.1°, α 95 = 7.0°, and k = 23.9, indicating virtually no rotation with respect to a reference paleomagnetic direction for the Asian continent.
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