信江盆地是我国丹霞地貌发育最典型的区域之一。
The Xinjiang Basin is one of the typical areas in China where develop typical Danxia landforms.
晚白垩世信江盆地北缘及南缘边界断层附近发育冲积扇体系，中央洼陷区发育河流沉积体系。
Fluvial fan sedimentary system disposed at the edge of south and north basin; Braided river system disposed in the central basin in late cretaceous in Xinjiang.
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