高级搜索
    鞠文信, 苏士杰, 白翠霞, 邵军. 大兴安岭乌尔旗汉地区晚石炭世半拉山序列侵入岩特征[J]. 地质与资源, 2005, 14(3): 161-165. DOI: 10.13686/j.cnki.dzyzy.2005.03.001
    引用本文: 鞠文信, 苏士杰, 白翠霞, 邵军. 大兴安岭乌尔旗汉地区晚石炭世半拉山序列侵入岩特征[J]. 地质与资源, 2005, 14(3): 161-165. DOI: 10.13686/j.cnki.dzyzy.2005.03.001
    shu
    JU Wen-xin, SU Shi-jie, BAI Cui-xia, SHAO Jun. CHARACTERISTICS OF THE LATE CARBONIFEROUS BANLASHAN SERIES OF INTRUSIVE ROCKS IN ORQOHAN AREA, DAHINGGANLING[J]. Geology and Resources, 2005, 14(3): 161-165. DOI: 10.13686/j.cnki.dzyzy.2005.03.001
    Citation: JU Wen-xin, SU Shi-jie, BAI Cui-xia, SHAO Jun. CHARACTERISTICS OF THE LATE CARBONIFEROUS BANLASHAN SERIES OF INTRUSIVE ROCKS IN ORQOHAN AREA, DAHINGGANLING[J]. Geology and Resources, 2005, 14(3): 161-165. DOI: 10.13686/j.cnki.dzyzy.2005.03.001
    shu

    大兴安岭乌尔旗汉地区晚石炭世半拉山序列侵入岩特征

    CHARACTERISTICS OF THE LATE CARBONIFEROUS BANLASHAN SERIES OF INTRUSIVE ROCKS IN ORQOHAN AREA, DAHINGGANLING

      摘要
    • 摘要: 晚石炭世侵入岩与得尔布干成矿带多金属成矿有密切成因联系.从半拉山侵入岩序列的地质特征和岩石地球化学特征探讨了晚石炭世侵入岩的形成环境和侵位机制,认为半拉山序列侵入岩是地幔成分为主的混合来源,形成于俯冲作用环境.

       

      Abstract: The Late Carboniferous intrusive rocks in Orqohan area are closely related to the polymetal minerogenesis of Derbugan metallogenic belt. The forming environment and mechanism of the rocks are discussed by studying on the geological and geochemical characteristics of Banlashan series. It is concluded that the intrusive rocks of Banlashan series are evolved from the mixed materials of meanly mantle source, and intruded in subduction area.

       

      • HTML全文
      • 参考文献(0)
      • 相关文章
      • 施引文献
    • 资源附件(0)

    /

    返回文章
    返回