1) plate accretion in South China
华南板块汇聚
2) South China Plate
华南板块
1.
The evolution of sedimentation of South China plate in the Hercynian Indosinian stage can be divited into five substages from its occurrence to subduction, which corresponds to Ⅱ cycle of the relative sea level change, and the Dongwu movement is the turning point, which took place between the Early and Late Permian.
华南板块在海西—印支期的沉积演化，可以分为从发展到消亡的五个亚阶段，并和海平面相对升降的Ⅱ级旋回相当，早晚二叠世间的东吴运动是这个阶段由发生到衰亡的转折点。
2.
The junction belt between the Yangtze plate and South China plate passes central Jiangxi.
扬子板块与华南板块对接带由江西中部通过,其中萍乡地区自燕山运动末期以来,在北部以逆冲推覆作用为主,形成了大规模的逆冲推覆构造,南部在重力滑脱作用下,形成变质—岩浆热穹隆和一系列滑褶构造带及滑块构造,中部则形成相互叠覆的南、北构造对接带。
4) South China
华南微板块
1.
Review on Rodinia and Tectonics in South China;
Rodinia裂解与华南微板块形成和演化
5) Southern part of the North China plate
华北板块南部
6) the north margin of Huanan Plate
华南板块北缘
1.
Domal deformational-metamorphic body which developed in Wugongshan region of Pingxiang City, Jiangxi Province in the north margin of Huanan Plate belongs to magmatic core complexes.
华南板块北缘江西萍乡武功山地区发育的穹窿状变形变质体属岩浆核杂岩,其结构特征和成因机制,与经典的变质核杂岩有相似之处,但其核部是花岗岩,它主要是花岗岩浆强力底辟侵位引起地壳局部隆升和伸展滑覆。
补充资料：汇聚
同‘会聚 ’。
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参考词条