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Fig. 8 | Swiss Journal of Geosciences

Fig. 8

From: Vertical-axis rotation in East Kopet Dagh, NE Iran, inferred from paleomagnetic data: oroclinal bending or complex local folding kinematics?

Fig. 8

Cross-component IRM thermal demagnetization curves for three selected samples. Soft, medium and hard coercivity fractions relate to 0.1, 0.3 and 1.2 T, respectively. a, b Samples P01b and P05c (Pestehleigh Formation: continental red beds) show a mixture of low-coercivity magnetite and hematite with a large range of coercivities. c Sample P07e (Chehel Kaman: white carbonates) indicates low- to medium-coercivity magnetite as magnetic carrier

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