Authigenic mineral assemblage formed in different ambients is distinct to each other. 两种环境下形成的自生矿物组合截然不同。
This effect results from the transformation of original clay minerals in the rocks and the recryst allisation and reorientation of new mineral phases. 这一效果来源于岩石中原始粘土矿物的改变和新生矿物相的重结晶和重新取向。
