northern margin of Yangtze plate 扬子板块北缘
paleo-yangtze plate 扬子板块
the northern yangtze plate 扬子陆块北缘
west margin of yangtze plate 扬子板块西缘
western margin of yangtze plate 扬子板块西缘
yangtze paleo-plate 扬子古板块
The formation of the Qinling orogeny belt. experienced an endless geological periodand it was the result of combined action between the North China plate and Yangtze plate.
秦岭造山带的形成经历了漫长的地质历史,主要是古生代华北板块和扬子板块联合作用的结果,秦岭造山带的构造演化以及构造单元的划分尚存在较多分歧。
参考来源 - 南秦岭构造带旬阳—神河一带地质构造特征·2,447,543篇论文数据，部分数据来源于NoteExpress
The Bikou terrane lies at the junction of Qinling orogenic belt, Songpan-Garze orogenic belt and Yangtze Plate.
碧口地块位于秦岭—大别、松潘—甘孜造山带与扬子板块的交汇部位。
The study area is in the middle of Ningzhen Mountains which is located in the adjoining region of Yangtze plate and North China plate.
宁镇山脉中段位于中国东部陆壳扬子壳块东段北缘与华北壳块东段南缘相接地带。
Dg Zhongdian microplate was split off from the western margin of the Yangtze plate as the Garz Litang ocean opened in the late Permian.
德格—中甸微板块是在晚二叠世初随甘孜—理塘洋的产生而从扬子板块西缘分离出来的。
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