1.The sediments are detrital and largely of greywacke facies.

1.沉积岩为质，大于杂质砂岩相。

2.Glauconite, detrital carbonate skeletal debris, marine fossils, and collophane are commonly present.

2.海绿石、碳酸盐骨骸、海相化石和胶磷矿普遍出现。

3.The albite component increases while anorthic component decreases in detrital plagioclase.The plagioclase turned into an end - member component of albite.

3.斜长石钠长石组逐渐增多，钙长石组逐渐减少，最终形成纯钠端元的钠长石。