西伯利亚板块是世界上古老的地质构造单元之一。
The Siberia plate is one of the old geological structure units in the world.
板块之间采用插接方式连接，能吸收层间变位及单元变形，可承受较大幅度建筑物移动。
Socket joint is adopted between the plates, which can allow the inter-story drift and unit deformation and withstand substantial building movement.
扬子地块西南缘，属华南板块南部，跨扬子陆块和南华活动带两个大地构造单元。
SW Margin of the Yangtze Block, belonged to South part of the South China Plate, spans two geotectonic units of Yangtze Landmass and South China active zone.
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