碳酸盐岩深覆盖区隐伏岩溶构造的音频大地电磁探测:以云南大关地区为例

王桥, 杨剑, 唐发伟, 夏时斌, 廖国忠, 张伟, 李华, 高慧. 2023. 碳酸盐岩深覆盖区隐伏岩溶构造的音频大地电磁探测:以云南大关地区为例. 沉积与特提斯地质, 43(4): 770-778. doi: 10.19826/j.cnki.1009-3850.2021.08012
引用本文: 王桥, 杨剑, 唐发伟, 夏时斌, 廖国忠, 张伟, 李华, 高慧. 2023. 碳酸盐岩深覆盖区隐伏岩溶构造的音频大地电磁探测:以云南大关地区为例. 沉积与特提斯地质, 43(4): 770-778. doi: 10.19826/j.cnki.1009-3850.2021.08012
WANG Qiao, YANG Jian, TANG Fawei, XIA Shibin, LIAO Guozhong, ZHANG Wei, LI Hua, GAO Hui. 2023. Audio magnetotelluric detection of hidden karst in deep carbonate coverage area: A case study of Daguan area in Yunnan province, China. Sedimentary Geology and Tethyan Geology, 43(4): 770-778. doi: 10.19826/j.cnki.1009-3850.2021.08012
Citation: WANG Qiao, YANG Jian, TANG Fawei, XIA Shibin, LIAO Guozhong, ZHANG Wei, LI Hua, GAO Hui. 2023. Audio magnetotelluric detection of hidden karst in deep carbonate coverage area: A case study of Daguan area in Yunnan province, China. Sedimentary Geology and Tethyan Geology, 43(4): 770-778. doi: 10.19826/j.cnki.1009-3850.2021.08012

碳酸盐岩深覆盖区隐伏岩溶构造的音频大地电磁探测:以云南大关地区为例

  • 基金项目: 中国地质调查局地质调查项目(DD20230238,DD20190033);国家自然科学基金(41804144)
详细信息
    作者简介: 王桥(1984—),博士,高级工程师,主要从事地球物理应用及研究工作。E-mail:540363176@qq.com
  • 中图分类号: P31

Audio magnetotelluric detection of hidden karst in deep carbonate coverage area: A case study of Daguan area in Yunnan province, China

  • 碳酸盐岩受水溶蚀易于发育岩溶,形成溶洞、地下河等,常导致油气钻探出现掉钻、卡钻等情况。调查和研究显示,云南大关地区奥陶系五峰—志留系龙马溪组富有机质页岩具有高含气性,是勘探开发的重要领域。然而,该地区分布的二叠系茅口组和栖霞组碳酸盐地层广泛发育岩溶构造,这在很大程度上制约了页岩气的进一步勘探。同时,这两套地层的埋深可能超过1 km,对地球物理方法的探测精度也提出了挑战。本文通过理论模型试算和已有钻孔(D0)的方法试验,明确了音频大地电磁方法识别深部隐伏岩溶的可行性。在预选井位区(D1)开展音频大地电磁探测,并根据电性模型重新部署了调查井(D2),实际钻井检验了方法的可靠性,并认为不连续分布的高电阻率异常区往往指示岩溶构造的存在,井位布设的有利区可能是高电阻率异常连续分布的块状或带状异常区。因此,音频大地电磁探测不仅对岩溶覆盖区的油气钻井选址具有先导作用,同时也拓宽了该方法的应用范围。

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  • 图 2  研究区地质图

    Figure 2. 

    图 1  四川盆地及周缘地区碳酸盐岩分布(a;据陈阵,2017修改)及研究区岩性柱状图(b)

    Figure 1. 

    图 3  理论试算模型及响应

    Figure 3. 

    图 4  CC’剖面电性结构及解释

    Figure 4. 

    图 5  AA’剖面电性结构及解释

    Figure 5. 

    图 6  BB’剖面电性结构及解释

    Figure 6. 

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出版历程
收稿日期:  2021-03-25
修回日期:  2021-07-13
录用日期:  2021-08-03
刊出日期:  2023-12-31

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