LIN Min. 2018: New progress in the study of stratigraphic sequence and epoch of Baiyin'gaolao Formation in Demohada basin, Inner Mongolia. Geological Bulletin of China, 37(9): 1588-1598.
    Citation: LIN Min. 2018: New progress in the study of stratigraphic sequence and epoch of Baiyin'gaolao Formation in Demohada basin, Inner Mongolia. Geological Bulletin of China, 37(9): 1588-1598.

    New progress in the study of stratigraphic sequence and epoch of Baiyin'gaolao Formation in Demohada basin, Inner Mongolia

    • The Demohada volcanic-eruption basin is one of the most important Late Mesozoic volcanic basins in southern Da Hinggan Mountains. It is considered that the Demohada volcanic-eruption basin is composed of volcanic rocks of Baiyin'gaolao Formation, which is divided into three lithologic segments and constitutes a total sedimentary and eruption cycle. The volcanic rocks have eight types with nine Ⅴ-grade volcanic apparatuses, obviously controlled by NNE-trending faults. The results of zircon U-Pb dating show that the volcanic activity of the basin occurred mostly from 128Ma to 125Ma, suggesting Early Cretaceous.
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