拉萨地体和羌塘地体新生代内部变形较小。
The Cenozoic internal deformation in Qiangtang and Lhasa terranes is not serious.
适应于湿透的土壤，这物种经验在塘地是填满的或者转向地下水。
Adapted to soggy soils, the species suffers where wetlands are filled or groundwater is diverted.
红河断裂带两侧古地磁结果表明，羌塘地体与扬子地台至少从早白垩世以来已连接为一个整体。
Paleomagnetic results from the both sides of Honghe fault zone have shown that the Yangzi block has been united with the Qiangtang terrane since Cretaceous.
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