任楼煤矿二叠系石河子组含煤岩系旋转的天文周期驱动

IF 2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Guodong Shi , Duoxi Yao , Xuekuan Shi
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引用次数: 0

摘要

任楼煤矿海陆过渡沉积岩发育于含煤岩层中,具有明显的周期性。这些沉积周期与天文周期信号具有良好的对应关系。本文对任楼煤矿地层进行了周期分析。首先,根据 Laskar J 和 Waltham 的算法确定了从 289 Ma 到 293 Ma 的地球轨道参数变化周期。同时还计算了这一沉积时期米兰科维奇周期的理论周期率。其次,利用 Acycle 软件对任楼矿区四个钻孔(S1-S4)的 GR 测井数据进行了旋回地层分析。最后,以 S1 钻孔 1007.93 m 处的 293 Ma 为锚点,利用 405 ka 长偏心率进行天文调谐,建立了浮动天文年代尺度。结果表明,任楼煤矿二叠系上、下石河子地层含煤岩系明显受米兰科维奇周期的控制和驱动。其周期参数与二叠纪天文轨道周期周期接近。旋回地层机理的研究对探索矿井地质灾害的机理和防治具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Astronomical cycle driving of coal-bearing rock system rotations in the Permian Shihezi Formation at Renlou Coal Mine
Marine terrestrial transitional sedimentary rocks of Renlou Coal Mine are developed in coal bearing rock formations, which exhibits obvious cyclicity. These sedimentary cycles have a good correspondence with astronomical cycle signals. This paper provides a cyclic stratigraphy analysis of Renlou Coal Mine. First, the period of change of the Earth's orbital parameters from 289 to 293 Ma are determined based on the algorithm of Laskar J and Waltham. The theoretical period ratio of Milankovitch's cycles during this depositional period is also calculated. Second, the GR logging data from the four boreholes of the Renlou Mine (S1–S4) are analysed for cyclothem stratigraphy by Acycle software. Finally, a floating astronomical dating scale was established with S1 borehole 1007.93 m at 293 Ma as an anchor point by using 405 ka long eccentricity for astronomical tuning. The results show that the coal-bearing rock systems of the Permian Upper and Lower Shihezi Formations in Renlou Coal Mine are obviously controlled and driven by Milankovitch cycles. The cycle parameters are close to the Permian astronomical orbital cyclic cycle. The study of the mechanism of the cyclostratigraphy is of great significance for exploring the mechanism and prevention of geological hazards in mines.
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来源期刊
Solid Earth Sciences
Solid Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.60
自引率
5.00%
发文量
20
审稿时长
103 days
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