稀土组成模式及稀土元素配分模式图表明是较典型的海相沉积物稀土配分模式。
The composition mode of REE and distribution mode of REE show that this mode of distribution of REE is typical Marine deposit and belongs to genesis of Marine deposit.
一般为玄武岩、页岩发育的土壤可提取态钛含量高于花岗岩、砂岩、浅海相沉积物发育的土壤；
In general, contents of extractable Ti of soils from basalt and shale are higher than those from granite, sandstone, and shallow sea deposits;
海绿石是海相沉积的指相矿物，通常形成于海进系列，与低的沉积物供应速率有关。
Glauconite as a typical facies mineral is generally regarded as accompanied with transgression sequence, with a low sedimentation rate.
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