Journal
GONDWANA RESEARCH
Volume 35, Issue -, Pages 180-191Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.gr.2015.05.002
Keywords
Tiaojishan Formation; North China Block; Paleomagnetism; Late Jurassic; Mongol-Okhotsk suture
Categories
Funding
- 973 Program [2013CB429800]
- SinoProbe [02]
- NSFC [40974035]
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A new paleomagnetic study on well-dated (similar to 155 Ma) volcanic rocks of the Tiaojishan Formation (Fm) in the northern margin of the North China Block (NCB) has been carried out. A total of 194 samples were collected from 26 sites in the Yanshan Belt areas of Luanping, Beipiao, and Shouwangfen. All samples were subjected to stepwise thermal demagnetization. After removal of a recent geomagnetic field viscous component, a stable high temperature component (HTC) was isolated. The inclinations of our new data are significantly steeper than those previously published from the Tiaojishan Fm in the Chengde area (Pei et al 2011, Tectonophysics, 510, 370-380). Our analyses demonstrate that the paleomagnetic directions obtained from each sampled area were strongly biased by paleosecular variation (PSV), but the PSV can be averaged out by combining all the virtual geomagnetic poles (VGPs) from the Tiaojishan Fm in the region. The mean pole at 69.6 degrees N/203.0 degrees E (A(95) = 5.6 degrees) passes a reversal test and regional tilting test at 95% confidence and is thus considered as a primary paleomagnetic record. This newly determined pole of the Tiaojishan Fm is consistent with available Late Jurassic poles from red-beds in the southern part of the NCB, but they are incompatible with coeval poles of Siberia and the reference pole of Eurasia, indicking that convergence between Siberia and the NCB had not yet ended by similar to 155 Ma. Our calculation shows a similar to 1600-km latitudinal plate movement and crustal shortening between the Siberia and NCB after similar to 155 Ma. In addition, no significant vertical axis rotation was found either between our sampled areas or between the Yanshan Belt and the major part of the NCB after similar to 155 Ma. (C) 2015 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
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