从区域看，金伯利岩岩带组成了一个帚状。
In the area, a brush structure is formed by kimberlite zone.
特征性的菌落颜色与帚状枝及分生孢子的产生有关。
The characterized color of the colony was caused by the production of penicillus and conidium.
新华夏系第二沉降带华北沉降区，广泛发育了帚状构造。
Brush structures are fully developed in the North China subsiding belt of the Neocathaysian system.
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