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    中国百强科技报刊

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    Volume 47 Issue 8
    Sep.  2022
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    Article Contents
    Wu Haibo, Wang Guochen, Hou Yanping, Shi Guanzhong, Jia Zhenzhen, Peng Wei, Zhang Haijun, 2022. Seismic Identification of the Jurassic Volcano-Sedimentary series in the Hailar Basin and Lithofacies Palaeogeography Reconstruction. Earth Science, 47(8): 3056-3072. doi: 10.3799/dqkx.2021.236
    Citation: Wu Haibo, Wang Guochen, Hou Yanping, Shi Guanzhong, Jia Zhenzhen, Peng Wei, Zhang Haijun, 2022. Seismic Identification of the Jurassic Volcano-Sedimentary series in the Hailar Basin and Lithofacies Palaeogeography Reconstruction. Earth Science, 47(8): 3056-3072. doi: 10.3799/dqkx.2021.236

    Seismic Identification of the Jurassic Volcano-Sedimentary series in the Hailar Basin and Lithofacies Palaeogeography Reconstruction

    doi: 10.3799/dqkx.2021.236
    • Received Date: 2021-09-08
    • Publish Date: 2022-09-25
    • Jurassic volcanic rocks of the Tamulangou Formation show great potential for oil and gas exploration, but it is not clear that the volcanic eruption cycles and paleogeography of the Tamulangou Formation, which restricts the exploration for volcanic reservoirs in the basin. Considering the complicated volcanic facies that are often fast changed and various volcanic edifices, this paper comprehensively analyzes outcrop investigation, volcanic U⁃Pb geochronology, drilling and logging, and seismic data, and uses the technology of seismic reflection features, time slice, three⁃dimensional visualization and Mean Square Root Amplitude property to identify volcano⁃sedimentary series, volcanic eruption cycles and lithological paleogeography of each sag in Hailaer Basin. These lines of evidence suggest that Jurassic rocks in Hailaer Basin developed two sets of volcanic⁃sedimentary cycles. Sedimentary beds that deposited outside volcanic edifices during the intermittent period of volcanic eruptions are used as mark beds to regionally recognize eruption cycles due to the continuous reflections formed on the corresponding seismic profile. The Mean Square Root Amplitude that is sensitive to lithology is used to outline volcanic edifices and their surrounding sedimentary beds. The first volcanic⁃sedimentary cycle is characterized by mafic to acidic volcanic rocks and sedimentary intervals that correspond to the Tamulangou Formation outside of the basin. The second volcanic⁃sedimentary cycle is characterized by acidic volcanic rocks and sedimentary intervals, corresponding to the Manitu Formation outside of the basin. The western depression zone mainly develops volcanic edifices and volcanic⁃sedimentary aprons at the edges of the volcanic edifices. The central and eastern depression zones mainly develop lacustrine sandstone and mudstone. The volcanic edifices inside sags are mainly concentrated in the basin floor or slope zone. The Jurassic volcanic⁃sedimentary rocks in the Hailar Basin shows typical characteristics of fault⁃control lake basins, and the Erguna and Deerbugan fault zones in the region greatly influence the distribution of volcanic⁃sedimentary rocks.

       

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