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     The geotectonic and kinetic characteristics of decollement and decouple structures in the Dingxiang areahave been studitvi, and the author has drawn a conclusion that the decollement and decouple structures system belongs tothe back margin stretching belt and part of tlie middle transitional belt between the Jiangnan paleo-continent and theYangtze River.
     本文探讨了丁香地区滑脱拆离构造的几何学、运动学特征,并初步厘定该地区的滑脱拆离属于江南古陆北侧、长江以南整体滑覆-剥离断层体系的后缘位伸带及中间过流带之部分。
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     prostrate,D.
     俯和 D.
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     GEOCHEMICAL POTENTIAL
     地球化学
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     ④Osteophyte formation of the vertebrae.
     4 )椎体后缘骨赘 ;
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     The stresses in sitting position were smaller and the distribution was more even than those in bilateral leg standing position.
     单腿站立时的应力值大于双腿站立,尤其是在关节面的前后缘
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     The posterior vertebral body-height was decreased in six patients.
     侧X线片示骨折椎体楔形变,其中6例椎体后缘高度有丢失。
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The geotectonic and kinetic characteristics of decollement and decouple structures in the Dingxiang areahave been studitvi, and the author has drawn a conclusion that the decollement and decouple structures system belongs tothe back margin stretching belt and part of tlie middle transitional belt between the Jiangnan paleo-continent and theYangtze River.The decollement and decouple structures of Dingxiang area have been divided into one underlying system,four decollement and decouple layer systems,four main...

The geotectonic and kinetic characteristics of decollement and decouple structures in the Dingxiang areahave been studitvi, and the author has drawn a conclusion that the decollement and decouple structures system belongs tothe back margin stretching belt and part of tlie middle transitional belt between the Jiangnan paleo-continent and theYangtze River.The decollement and decouple structures of Dingxiang area have been divided into one underlying system,four decollement and decouple layer systems,four main decollement and decouple planes and eight Subordinate decolle-ment and decouple planes.Combining with the regional development,the forming conditions andevolution of the decolle-ment and decouple structu res have also been discussed.

本文探讨了丁香地区滑脱拆离构造的几何学、运动学特征,并初步厘定该地区的滑脱拆离属于江南古陆北侧、长江以南整体滑覆-剥离断层体系的后缘位伸带及中间过流带之部分。文章把丁香地区滑脱拆离构造划分出下伏系统。四个滑脱拆离层系及四个主滑脱拆离面和八个次滑脱拆离面。结合区域地质发展史,还对滑脱拆离构造的成因及其演化做了讨论。

 
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