Paleomagnetic Study of Shanwang Formation, Shandong Province, China.

摘要

The measured direction of the stable remanence of Shanwang Formation, Shandong Province, is D = 355.8 deg., I = 47.1 deg. According to the axial geocentre dipole model, the paleolatitude there during Miocene was 28.3 deg. N. The corrected value based on far-sided effect is 32.4 deg. N. The uncorrected and corrected pole positions were (81.0 deg. N, 323.1 deg. E) and (84.6 deg. N, 339.7 deg. E) separately. Comparing them with paleo-flora shows that the corrected value of paleolatitude is probably reasonable. (author). 14 refs, 3 figs, 1 tab. (Atomindex citation 20:052017)