Cretaceous paleomagnetism of the Methow-Pasayten belt, Washington

Mathematics – Logic

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Geomagnetism, Paleomagnetism, Remanence, Structural Properties (Geology), British Columbia, Geological Faults, Sites, Tectonics, Washington

Scientific paper

Detailed demagnetization experiments isolated a characteristic remanent magnetization in ten stable sites from the upper Cretaceous Winthrop and Midnight Peak Formations in the Methow-Passayten belt of north-central Washington. This remanence agrees best between opposite limbs of a fold (the Goat Peak syncline) when corrected for 46 percent of tilt. This is consistent with magnetization acquired during deformation. Synfolding magnetization may have been facilitated by a thermochemical event associated with synkinematic intrusions along the axis of folding. The mean direction (D = 12.0 deg, I = 61.1 deg, Alpha-95 = 4.8 deg) is highly discordant with respect to the expected direction for north-central Washington. This discordance points to about 1,400 km of poleward transport and 48 deg of clockwise rotation between 93 and 45-48 Ma.

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