赵隆业, 陈基娘, 王天顺. 关于中国油页岩的工业成因分类[J]. 煤田地质与勘探, 1991, 19(5): 2-6.
引用本文: 赵隆业, 陈基娘, 王天顺. 关于中国油页岩的工业成因分类[J]. 煤田地质与勘探, 1991, 19(5): 2-6.
ZHAO Long-ye, CHEN Ji-niang, WANG Tian-shun. INDUSTRIAL-ORIGINAL CLASSIFICATION OF CHINESE OIL SHALES[J]. COAL GEOLOGY & EXPLORATION, 1991, 19(5): 2-6.
Citation: ZHAO Long-ye, CHEN Ji-niang, WANG Tian-shun. INDUSTRIAL-ORIGINAL CLASSIFICATION OF CHINESE OIL SHALES[J]. COAL GEOLOGY & EXPLORATION, 1991, 19(5): 2-6.

关于中国油页岩的工业成因分类

INDUSTRIAL-ORIGINAL CLASSIFICATION OF CHINESE OIL SHALES

  • 摘要: 我国还没有一个实用的油页岩工业成因分类,故影响到对其资源的评价。在评介国外油页岩分类的基础上,根据我国21个油页岩产地的样品分析测试资料,选择灰分产率、焦油产率、发热量、灰成分作为油页岩分类的指标。首先按油页岩的成因分为腐泥、腐殖腐泥、腐泥腐殖和腐殖残殖4类,以A、B、C、D表示;再按有机质成分分为3类,以10、20、30表示;还按无机质成分:硅质、硅铝质、铁质和钙质灰分分成4种,以1、2、3、4表示。

     

    Abstract: There has not been a particable industrial-original classification of oil shales in China as yet. Just because of this, the rational evaluation of oil-shale resource has been affected. On the basis of the appraisal for foreign classification and the analysical results of the samples obtained from 21 oil-shale producing areas, ash content, tar yield, calorific value and ash constituent are chosen as the parameters of classification. Oil shale is originally classified into sapropel(A), humics-sapropel(B), sapropelhumics(c) and liptobiolith(D). Then, it is divided three groups, stood for by 10,20 and 30, by orginic composition. Further, four varieties, symbolized separately by 1,2,3 and 4, are distinguished from inorganic composition i.e.ash type of silica, silica-alumina, iron or calcite.

     

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