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A study of magnetotelluric sounding of Xiushui Basin in the northern periphery of Liaohe |
Peng-Hui ZHANG1,2, Xiao-Bo ZHANG1,2, Yong-Zhen YUAN1,2, Hui FANG1,2, Jian-Xun LIU1,2, Chun-Xiang JIANG1,2 |
1. National Center for Geological Exploration Technology, Langfang 065000, China 2. Institute of Geophysical and Geochemical Exploration, Langfang 065000, China |
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Abstract Xiushui Basin is a small-sized Mesozoic fault depression located in the south of Zhangqiang fault depression where good indications of oil and gas have been drilled in its volcanic reservoirs in recent years. In order to find out the boundary, internal framework and stratigraphic distribution of the Xiushui Basin, the authors conducted magnetotelluric sounding and gravity and magnetic profile measurement along two survey lines and, as a result, obtained the magnetic anomaly curves and the shallow electrical structures of the Xiushui Basin and its peripheral east and west sides. Constrained by drilling, geological and petrophysical data, the electrical structure characteristics of strata in different ages were determined, and the regional geological-geophysical model was synthetically established. The results show that the overall caprock of Xiushui Basin has low resistivity, which is apparently different from that of underlying basement. The basement of Xiushui Basin consists mainly of Upper Paleozoic strata, and the composition of the basement in the north is different from that in the south. In addition, the basement on east and west sides of the periphery of the basin consists of Precambrian metamorphic rock series. The basin has a structural pattern of two concaves and one uplift, relatively larger in the eastern sub-depression. The understanding obtained by the authors provides reliable geophysical basis for the oil and gas resources evaluation in the Xiushui Basin and Mesozoic basins in the periphery of the Songliao Basin.
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Received: 20 February 2019
Published: 25 October 2019
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Regional geology and magnetotelluric sounding profile location in Xiushui Basin
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地层 | 岩石样品测试 | MT首支视电阻率 | 岩性 | 数量 | 数值范围/(Ω·m) | 平均值/(Ω·m) | 数量 | 数值范围/(Ω·m) | 平均值/(Ω·m) | 第四系 | | | | | 6 | 6.7~77.8 | 29.9 | | | | | | 3 | | | | 安山玢岩 | 6 | 2564.1~6324 | 3980.0 | | | | | 安山岩 | 11 | 103~879.8 | 402.0 | | | | 白垩系义县组 | 安山玄武岩 | 6 | 1166~4832 | 2190.0 | 62 | 14.9~81.9 | 24.5 | | 辉绿岩 | 6 | 224~711 | 397.0 | | | | | 粉砂岩 | 11 | 218~601 | 372.0 | | | | 侏罗系 | 泥质粉砂岩 | 8 | 429~886 | 515.0 | 7 | 73.1~172.9 | 121.7 | | 花岗岩 | 12 | 1506~4300 | 2820.0 | | | | 石炭—二叠系 | | 68 | 994~10764 | 3964.0 | 9 | 154.9~322.5 | 246.9 | 元古宇 | | | | | 1 | | 105.7 | 侵入岩 | | | | | 19 | 105.6~543 | 287.4 |
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Analysis results of resistivity parameters for field rocks and first branch resistivityparameters for magnetotelluric sounding
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Comparison of resistivity log and near-well bathymetric data in Xiushui basin
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地层 | 主要岩性 | 样品数 | 最小值/(g·cm-3) | 最大值/(g·cm-3) | 平均值/(g·cm-3) | 白垩系 | 粉砂岩、泥质粉砂岩 | 11 | 2.46 | 2.68 | 2.59 | 2.61 | 花岗岩 | 5 | 2.46 | 2.64 | 2.58 | 安山岩、玄武质安山岩 | 12 | 2.47 | 2.61 | 2.54 | 玄武岩、安山质玄武岩 | 15 | 2.54 | 2.75 | 2.67 | 侏罗系 | 泥质粉砂岩、粉砂岩 | 6 | 2.46 | 2.70 | 2.58 | 2.62 | 花岗岩、二长花岗岩 | 14 | 2.55 | 2.66 | 2.60 | 石炭—二叠系 | 花岗岩、二长花岗岩 | 24 | 2.53 | 2.71 | 2.61 | 2.71 | 变质英安岩 | 15 | 2.65 | 2.90 | 2.76 | 石英岩 | 14 | 2.70 | 2.81 | 2.74 | 糜棱岩 | 11 | 2.71 | 2.86 | 2.77 |
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Analysis results of density parameters for field rocks
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Apparent resistivity curves for MT station along the profile
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Statistical rose diagrams of multi-measuring point multi-frequency point major electrical axis based on decomposition of the impedance tensor
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Gravity anomaly curve(a)、Magnetotelluric sounding two-dimensional inverted electrical section(b) and geological interpretation(c)of L1 line
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Gravity anomaly curve(a)、Magnetotelluric sounding two-dimensional inverted electrical section(b) and geological interpretation(c)of L2 line
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