景贵飞, 王式光. 宁武──静乐盆地中部煤系高岭岩的特征及成因[J]. 煤田地质与勘探, 1995, 23(1): 1-8.
引用本文: 景贵飞, 王式光. 宁武──静乐盆地中部煤系高岭岩的特征及成因[J]. 煤田地质与勘探, 1995, 23(1): 1-8.
Jing Guifei, Wang Shiguang. GEOCHEMISTRY AND ORIGIN OF TONSTEINS IN MIDDLE OF NINGWU-JINGLE BASIN, SHANXI PROVINCE[J]. COAL GEOLOGY & EXPLORATION, 1995, 23(1): 1-8.
Citation: Jing Guifei, Wang Shiguang. GEOCHEMISTRY AND ORIGIN OF TONSTEINS IN MIDDLE OF NINGWU-JINGLE BASIN, SHANXI PROVINCE[J]. COAL GEOLOGY & EXPLORATION, 1995, 23(1): 1-8.

宁武──静乐盆地中部煤系高岭岩的特征及成因

GEOCHEMISTRY AND ORIGIN OF TONSTEINS IN MIDDLE OF NINGWU-JINGLE BASIN, SHANXI PROVINCE

  • 摘要: 通过对宁武-静乐盆地中部高岭岩的组成、产状及稀土和微量元素地球化学特征的研究,发现了K+Na+Ca、TiO2、Nb、Zr等与高岭石含量间的正相关关系,讨论了细粒沉积物于沼泽中可能的沉降与扩散机制,认为研究区高岭岩为阴山古陆酸性陆源岩风化产物经搬运沉积后,又在沼泽环境中经淋滤进-步富集而成。

     

    Abstract: On the studies of the occurences, compositions and geochemical characteristics of the tonsteins in middle of Ningwu-Jingle Basin, We found the positive correlations between elements of Nb,Zr, (K + Na +Ca) and TiO2 and the contents of kaolinite, discussed the probable sedimentary and spreading mechanisms of fine-grained sediments in swamp,as well as proposing the view that the local tonsteins were formed by leaching and concentration of the weathering products of medi-acid igneous rocks of Yinshan palaeoland which were transported and sedimented in swamp.

     

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