俯冲造山带
The tectonic boundary between the Yangtze Continent and Qinling orogenic belt is a thrust-strike slip tectonic zone rather than a intracontinental subduction zone.
扬子大陆与秦岭造山带之间的壳内构造边界不具陆内俯冲性质,而是逆冲推复一走滑构造带。
The main A-type subduction fault and large scale thin-skinned tectonics clearly reveal that the Yangtze Plate subsides towards Dabie orogenic belt.
鄂皖边界大别南缘主俯冲边界断层的存在以及扬子板块前陆盆地盖层大型薄皮构造,揭示扬子板块向大别造山带之下的A型俯冲。
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