Paleomagnetic result of the Lower-Cretaceous from Luanping basin, Hebei Province and its tectonic implications

A paleomagnetic study of about 95 samples from 16 sites sampled in the Early Cretaceous in Luanping basin in Hebei Province was reported. Stepwise thermal demagnetization was used to isolate magnetic components. Most samples have a characteristic direction with a high temperature component above 500℃. The tectonic\|corrected data are D =347 8°, I =50 4°, α 95 =7.1°, and the corresponding pole position is at 76.1°N, 346.3°E, with dp =6.4°, dm =3 8°,paleolatitude λ =31.1°N. This result indicates a counterclockwise post\|Cretaceous rotation of 30.7°±9.8° with respect to the stable Ordos basin in the west of North China Block, and a non\|significant northward motion. This rotation could be related to local fault action or structural detachment, or regional NNW\|NWWward motion and collision of Kula\|Pacific plate with eastern China since the Early Cretaceous.