The form of secondary minerals is schistose aggregated and spherical.
次生矿物形态主要呈片状集合体和球状体。
Typically the rock is massive, but commonly it is flaggy or schistose.
这类岩石典型地呈块状，但常呈薄板状或片理化。
In addition, the large particles of the schistose crystals exhibit wave-shaped bending.
晶体呈定向排列，颗粒较大的片状晶体产生波状弯曲现象。
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