Further paleomagnetic results from the ∼ 155 Ma Tiaojishan Formation, Yanshan Belt, North China, and their implications for the tectonic evolution of the Mongol-Okhotsk suture

被引：73

作者：

Ren, Qiang ^{[1
]}

Zhang, Shihong ^{[1
]}

Wu, Huaichun ^{[1
]}

Liang, Zhongkai ^{[1
]}

Miao, Xianjun ^{[1
]}

Zhao, Hanqing ^{[1
]}

Li, Haiyan ^{[1
]}

Yang, Tianshui ^{[1
]}

Pei, Junling ^{[2
]}

Davis, Gregory A. ^{[3
]}

机构：

[1] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Beijing 100083, Peoples R China

[2] CAGS, Inst Geomech, Key Lab Paleomagnetism, Beijing 100081, Peoples R China

[3] Univ Southern Calif, Dept Earth Sci, Los Angeles, CA 90089 USA

来源：

GONDWANA RESEARCH | 2016年 / 35卷

关键词：

Tiaojishan Formation; North China Block; Paleomagnetism; Late Jurassic; Mongol-Okhotsk suture; ASIAN OROGENIC BELT; POLAR WANDER PATH; SOUTH CHINA; GEOMAGNETIC-FIELD; SOLONKER SUTURE; INNER-MONGOLIA; VOLCANIC-ROCKS; MAJOR BLOCKS; THRUST BELT; NE CHINA;

D O I：

10.1016/j.gr.2015.05.002

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

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.

引用

页码：180 / 191

页数：12

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