| 释义 |
glauconite 英/ ?ɡl??k??na?t / 美/ ?ɡl??k??na?t / - 1
地球科学 海绿石 Glauconite as a typical facies mineral is generally regarded as accompanied with transgression sequence,with a low sedimentation rate. 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。 海绿石灰岩
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The Phanerozoic glauconites in this study show that they were formed in an environment of weak reduction and low sedimentation. 显生宙的海绿石，多年来研究的结果表明海绿石发育在慢速弱还原环境。 - 2
We found that concentration areas of. Glauconites are identical with the oxidizing environment, coarse-sediment areas and relict sediments. 海绿石的富集区与氧化环境，粗粒沉积和残留沉积区相一致。 - 3
Therefore, all the evidence above suggests that geochemical facies for the glauconites should have been built in the nonmarine or lake environment. 因此，在陆相湖泊三角洲环境中，也应当建立海绿石地球化学相。
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