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《Quaternary Sciences》 2001-06
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Li Wanlun ① Lu Yanchou ① Ding Guoyu ② (① Institute of Geology, China Seismological Bureau, Beijing 100029; ② Center for Analysis and Prediction, China Seismological Bureau, Beijing 100036)  
Loess recorded stable detrimental remanent magnetization (DRM). It is possible to reveal the relative motion between the Ordos and its adjacent blocks by using the VGP (virtual geomagnetic pole) method in loess. Our preliminary results indicate that the Ordos block had rotated counterclockwise during the Quaternary period. Since 0.46MaB.P., its rotation relative to the Taihangshan block has been about 8.2°±5.8° and its rotation relative to the Xining block about 10.5°±6.4°. Its rotation relative to the Xining block has been about 29.8°±14.7° since 1 17MaB.P. and about 31.5°±11.4° relative to the Qinling block since 2.5MaB.P. From these results, the following estimates can be obtained: (1) there has been about 31.7km dextral slip along the western edge of the Ordos block (Liupanshan fault zone) since 1.17MaB.P.; (2) about 27.5km sinistral slip along the Weihe fault-bounded zone since the early Pleistocene (ca. 2.5MaB.P.); and (3) about 10.7km dextral slip along the Shanxi fault-bounded zone since 0.46MaB.P.
【Fund】: 国家自然科学基金项目 (批准号 :4 9732 0 90和 4 9872 0 6 2 )资助
【CateGory Index】: P542;P318
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