苏鲁造山带北侧构造演化的几何学运动学特征

吴冲龙; 张善文; 毛小平; 柳忠泉; 宋立军; 佟彦明

Volume 31 Issue 6

Jun. 2006

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Article Navigation > Earth Science > 2006 > 31(6): 817-822

WU Chong-long, ZHANG Shan-wen, MAO Xiao-ping, LIU Zhong-quan, SONG Li-jun, TONG Yan-ming, 2006. Geometry and Kinematics of Tectonic Evolution in Northern Part of Sulu Orogenic Belt. Earth Science, 31(6): 817-822.

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Geometry and Kinematics of Tectonic Evolution in Northern Part of Sulu Orogenic Belt

Received Date: 2006-02-26
Publish Date: 2006-11-25

Abstract

Abstract

Three layers are present in the middle and upper crusts in the northern border of Sulu orogenic belt, as revealed by the S-N-strike reflecting seismic profiles that cross the Zhucheng sag. These three layers are the uppermost sedimentary cover of Jiaolai basin, the Sulu sphenoid terrane in the middle layer and the Jiaobei terrane representing North China plate at the bottom. The fringe of Zhucheng sag and the interior fault are characterized by the syndeposit normal fault. A group of imbricated reverse thrust facing upward to the north has developed in Sulu sphenoid terrane, but the Jiaobei terrane has the trend of subducting to the south. As a result, a collision mechanism is perhaps present between continents where North China plate and Yangtze plate subducted to each other below the Sulu terrene which has the same flower-shape orogenic structure as that of Dabie terrane.
- Sulu orogenic belt,
- Zhucheng sag,
- Jiaolai basin,
- geometry characteristics,
- kinematics characteristics,
- collision between continents,
- structure of orogenic belt.

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References(37)

References

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Geometry and Kinematics of Tectonic Evolution in Northern Part of Sulu Orogenic Belt

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