东准噶尔双泉一带的韧-脆性剪切带是在板块结合带基础上，形成于陆-陆碰撞体制。
Basing on the combination of plates, ductile-brittle shear zone in the ShuangQuan area, Eastern JungGar forms in the system of continental - continental collision.
江西北部地处欧亚大陆板块东南沿海前陆推覆冲断带，与扬子、华夏古板块结合带叠加部位。
North Jiangxi area is located in the superimposed part of foreland nappe thrust zone of the southeast coast of Eurasian Contiental Plate and Yangzi and Precambrian Cathaysia Plates.
深部地质与地球物理资料显示区内两板块深部结合带位置可能与表层存在较大差异，更加深了板块边界划分研究的复杂程度。
Some subsurface geology and Geophysics data revealed the possible of large gap between the boundaries' location of surface and subsurface, made the issue much more complex.
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