海绿石、碳酸盐骨骸碎屑、海相化石和胶磷矿普遍出现。
Glauconite, detrital carbonate skeletal debris, Marine fossils, and collophane are commonly present.
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。
We found that concentration areas of. Glauconites are identical with the oxidizing environment, coarse-sediment areas and relict sediments.
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。
Therefore, all the evidence above suggests that geochemical facies for the glauconites should have been built in the nonmarine or lake environment.
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。
The Phanerozoic glauconites in this study show that they were formed in an environment of weak reduction and low sedimentation.
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.
在数量充分时，海绿石能形成为砂质、绿色的沉积物，如美国及英国的白垩纪绿砂。
In sufficient quantity, it can form a sandy, green deposit such as the Cretaceous greensands of the us and UK.
沉积物主要由陆源碎屑组成，其它的再沉积碎屑组份有鲕粒、化石碎屑、植物碎屑和海绿石等。
The main sediments are made up of terrigenous clastic deposits. Other resedimented clastic constituents are: ooid, fossil clasts, plant clasts and glauconite, etc.
大量的薄片鉴定资料表明，济阳坳陷沾车凹陷新生界地层中含有海绿石矿物，并且均为原生海绿石。
It is indicated that glauconites have been found in Cenozoic group strata in Zhan-che sag of Jiyang depression by a variety of thin section identification, and which are all in the primary state.
③矿物学方面，海绿石、菱铁矿结核、硼元素含量和碳氧同位素资料也表明沉积环境由海→陆的过渡性质。
In terms of mineralogy, glauconites, siderite nodules, boron contents and carbon isotopes also show that the sedimentary environment is transitional.
海蓝宝石：此石反映其惊人的海绿颜色。
Aquamarine: The name of this stone reflects its stunning sea-green color.
海蓝宝石：此石反映其惊人的海绿颜色。
Aquamarine: The name of this stone reflects its stunning sea-green color.
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