朱如凯. 桌贺地区石炭纪沉积与聚煤特征[J]. 煤田地质与勘探, 1994, 22(3): 1-5.
引用本文: 朱如凯. 桌贺地区石炭纪沉积与聚煤特征[J]. 煤田地质与勘探, 1994, 22(3): 1-5.
ZHU Ru-kai. THE CARBONIFEROUS SEDIMENTS AND COAL ACCUMULATION FEATURES IN ZHUOZI AND HELAN MOUNTAINS REGION[J]. COAL GEOLOGY & EXPLORATION, 1994, 22(3): 1-5.
Citation: ZHU Ru-kai. THE CARBONIFEROUS SEDIMENTS AND COAL ACCUMULATION FEATURES IN ZHUOZI AND HELAN MOUNTAINS REGION[J]. COAL GEOLOGY & EXPLORATION, 1994, 22(3): 1-5.

桌贺地区石炭纪沉积与聚煤特征

THE CARBONIFEROUS SEDIMENTS AND COAL ACCUMULATION FEATURES IN ZHUOZI AND HELAN MOUNTAINS REGION

  • 摘要: 桌子山—贺兰山地区石炭纪沉积了一套巨厚的碎屑岩层,含少量碳酸盐岩夹层。自下而上依次为中统靖远组、羊虎沟组和上统太原组。该沉积为一套包括水下三角洲平原,上、下三角洲平原等三角洲沉积体系。区内备组段均含煤,其中以上三角洲平原成煤条件最好,煤层稳定,厚度大。

     

    Abstract: The studing areas are located in Zhuozi and Helan Mountains region. Its carboniferous strata are mainly composed of elastic rocks, including a little of carbonate. The stratigraphic seguence is divided into the Jiangyuan Formation (C12). Yanghugou Formation (C22) and Taiyuan Formation (C3).The sedimentary factes are a typical delta depositinal system. The upper delta plain is the best coal-bearing environment.

     

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