The tectonic boundary between the Yangtze Continent and Qinling orogenicbelt 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。
2
The microfabric deformation structure of andalusite in the Harlik orogenicbelt is genetically related to the faulting-induced regional metamorphism caused by intracontinental A-type subduction.
东疆哈尔·里克造山带中红柱石的变形显微构造与区内A型俯冲引起的断裂区域变质作用有成因联系。
3
The main A-type subduction fault and large scale thin-skinned tectonics clearly reveal that the Yangtze Plate subsides towards Dabie orogenicbelt.