The sediments are detrital and largely of greywacke facies.

沉积为碎屑质，大部分属于杂质砂相。

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

海绿石、碳酸盐骨骸碎屑、海相石和胶磷矿普遍出现。

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

斜长石碎屑中钠长石组分逐渐增多，钙长石组分逐渐减少，最终形成纯钠端元的钠长石。

The sediments are detrital and largely of greywacke facies.

沉积岩为碎质，大部分属于杂质砂岩相。

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

海绿石、碳酸盐骨骸碎、海相石和胶磷矿普遍出现。

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

斜长石碎中钠长石组分逐渐增多，钙长石组分逐渐减少，最终纯钠端元的钠长石。

The sediments are detrital and largely of greywacke facies.

沉积为碎质，大部分属于杂质砂相。

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

海绿石、碳酸盐骨骸碎、海相石和胶磷矿普遍出现。

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

斜长石碎中钠长石组分逐渐增多，钙长石组分逐渐减少，最终形成纯钠端元的钠长石。

The sediments are detrital and largely of greywacke facies.

沉积岩为质，大部分属于杂质砂岩相。

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

海绿、碳酸盐骨骸、海相和胶磷矿普遍出现。

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

斜长中钠长组分逐渐增多，钙长组分逐渐减少，最终形成纯钠端元钠长。

The sediments are detrital and largely of greywacke facies.

沉积岩为质，大部分属于杂质砂岩相。

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

海绿石、碳酸盐骨骸、海相石和胶磷矿普遍出现。

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

斜长石中钠长石组分逐渐增多，钙长石组分逐渐减少，最终钠端元的钠长石。

The sediments are detrital and largely of greywacke facies.

沉积为碎质，大部分属于杂质砂相。

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

海绿石、碳酸盐骨骸碎、海相石和胶磷矿普遍出现。

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

斜长石碎中钠长石组分逐渐增多，钙长石组分逐渐减少，成纯钠端元的钠长石。

The sediments are detrital and largely of greywacke facies.

沉积岩为碎屑质，大部分属于杂质砂岩相。

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

海绿石、碳酸盐骨骸碎屑、海相石和胶磷矿普遍出现。

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

斜长石碎屑中钠长石分逐渐增多，钙长石分逐渐减少，最终形成纯钠钠长石。

The sediments are detrital and largely of greywacke facies.

沉积岩为碎质，大部分属于杂质砂岩相。

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

海绿石、碳酸盐骨骸碎、海相石和胶磷矿普遍出现。

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

斜长石碎中钠长石组分逐渐增多，钙长石组分逐渐减少，最终纯钠端元的钠长石。

The sediments are detrital and largely of greywacke facies.

沉积岩为碎质，大部分属于杂质砂岩相。

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

海绿、碳酸盐骨骸碎、海相和胶磷矿普遍出现。

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

斜碎中组分逐渐增多，钙组分逐渐减少，最终形成纯端元。

The sediments are detrital and largely of greywacke facies.

沉积岩为碎屑质，大部分属于杂质砂岩相。

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

海绿石、碳酸盐骨骸碎屑、海相石和胶磷矿普遍出现。

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

斜石碎屑中石分逐渐增多，钙石分逐渐减少，最终形成纯端元石。