庄军, 徐兢, 荀柏松, 滕辉, 余江滨. 硅藻土的成矿条件和资源评价[J]. 煤田地质与勘探, 1990, 18(2): 16-20.
引用本文: 庄军, 徐兢, 荀柏松, 滕辉, 余江滨. 硅藻土的成矿条件和资源评价[J]. 煤田地质与勘探, 1990, 18(2): 16-20.
THE FORMING CONDITIONS AND RESOURCE EVALUATION OF DIATOMITE[J]. COAL GEOLOGY & EXPLORATION, 1990, 18(2): 16-20.
Citation: THE FORMING CONDITIONS AND RESOURCE EVALUATION OF DIATOMITE[J]. COAL GEOLOGY & EXPLORATION, 1990, 18(2): 16-20.

硅藻土的成矿条件和资源评价

THE FORMING CONDITIONS AND RESOURCE EVALUATION OF DIATOMITE

  • 摘要: 对全国各主要硅藻土产地的成矿条件和硅藻植物的大最研究,发现硅薄土的厚度与古构造的活动频率有关。硅藻植物的种属、数量、壳体的完整性、繁衍速度和无机物质的种类、数量等与生境、沉积条件、水体的地球化学特征、古气候等有关。在此基础上总结出硅藻土资源评价的野外工作方法和室内研究重点。

     

    Abstract: Having made a great number of study on theforming conditions of diatoms in the principaldiatomite-produing areas, the authers foundthat the thickness of diatomite is related to thefrequenry of palaeo-structure activy。In an areawith stable structures, diatomile deposjis arethick. Generally,diatom planis enteaded waste-ly and abundant reserves exists, where the hasin and water area were large. The generaand species,quanlify test complefeness multi-plying speed oi dialom anc ihe varieties andquantity of inorganic subtance are related tothe environments iepositional conlitions,hydrochemicai features of waler body, palaeoclamit and other factors, From the study, thepaper deduced the field methods and labora-tory-research emphasisfor the diatomiteresources vealuation.

     

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