解光新. 陕西彬县大佛寺D4钻孔勘察地球化学研究[J]. 煤田地质与勘探, 2003, 31(4): 5-9.
引用本文: 解光新. 陕西彬县大佛寺D4钻孔勘察地球化学研究[J]. 煤田地质与勘探, 2003, 31(4): 5-9.
JIE Guang-xin. Exploration geochemistry research on Dafesi Borehole D4, Binxian, Shaanxi[J]. COAL GEOLOGY & EXPLORATION, 2003, 31(4): 5-9.
Citation: JIE Guang-xin. Exploration geochemistry research on Dafesi Borehole D4, Binxian, Shaanxi[J]. COAL GEOLOGY & EXPLORATION, 2003, 31(4): 5-9.

陕西彬县大佛寺D4钻孔勘察地球化学研究

Exploration geochemistry research on Dafesi Borehole D4, Binxian, Shaanxi

  • 摘要: 运用烃类勘察地球化学方法,对鄂尔多斯盆地南部彬县大佛寺井田钻遇中侏罗统煤层的D4钻孔,进行了垂向剖面多指标的综合地球化学研究。结果表明:剖面中所有岩样中的烃类物质均为热解烃生成初期演化阶段的煤成烃产物,具明显的同一性;由煤层至地表黄土,所有岩样中的烃类呈明显的、规律性垂直向上运移。这证实地下煤层烃类在近地表具有很好的地球化学信息显示,利用勘察地球化学方法找煤/煤层气是可行的。

     

    Abstract: With the hydrate exploration geochemistry method,it is conducted that the vertically cross section combined indexes geochemistry research on Jurassic coal beds met by Dafesi Borehole D 4 in Dafesi coal field.The results indicate that the hydrate material in all samples collected from cross section is the preliminary stage's hydrate products from coals,being of same characteristics;from coal bed up to surface soil the hydrate material of samples showed out the up migrating indicates.It is confirmed that hydrate of underground coal bed is of geochemistry indicating,therefore,it is feasible to find coal/coalbed gas with the methods of exploration geochemistry.

     

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