贺广田, 薛连明. 1986: 青海的石炭系. 地质通报, (3): 211-220.
    引用本文: 贺广田, 薛连明. 1986: 青海的石炭系. 地质通报, (3): 211-220.
    HE Guang-tian, XUE Lian-ming. 1986: THE CARBONIFEROUS SYSTEM OF QINGHAI PROVINCE. Geological Bulletin of China, (3): 211-220.
    Citation: HE Guang-tian, XUE Lian-ming. 1986: THE CARBONIFEROUS SYSTEM OF QINGHAI PROVINCE. Geological Bulletin of China, (3): 211-220.

    青海的石炭系

    THE CARBONIFEROUS SYSTEM OF QINGHAI PROVINCE

    • 摘要: 青海的石炭系分布广泛。北自祁连山、南至唐古拉;西自祁曼塔格,东至西倾山。以柴达木盆地周边的阿木尼克山、欧龙布鲁克山、布尔汗布达山、祁曼塔格和祁连山等地最为发育。青海石炭系的分布主要受古构造和地理环境所控制。沉积类型复杂,且各地发育程度不一。生物组合既有区域性生物面貌,又具明显的地方性特色。本文是依据广大地质工作者多年辛勤劳动之成果,结合笔者近年来参与区调及专题研究所收集的一些实际资料,对青海石炭系目前研究现状的扼要总结。文中采用石炭系二分方案,重点介绍青海石炭纪地层区划、地层系统及生物组合特征等。其它仅作简短讨论。

       

      Abstract: This paper briefly summarizes the present study of the Carboniferous System of Qinghai province. The province is stratigraphically divided into five regions, i. e. Qilian, Qaidam, Qingling, Bayan Har and Tanggula, and a number of subregions. With the section at the northeastern margin of the Qaidam basin as the type section of the Carboniferous of Qinghai, the Amunic, Fengshangou, Chengqianggou and hoit Taria Formations (Lower Carboniferous) and the Lower Hurleg, Upper Hurleg and Jabsar Gaxun Formations (Upper Carboniferous) have been established in ascending order. On the basis of the statistics of the range of occurrence of the biotas, the biostratigraphic sequ- ences of brachhiopods, corals and fusulinids have been set up. The characteris- tics of the rocks and strata and biotas of various formations are dealt with in details, and the upper and lower boundaries of the Carboniferous and the contact relationship between its upper and lawer series are also discussed briefly.

       

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