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    Volume 47 Issue 9
    Sep.  2022
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    Gao Wei, Shu Qing, Guo Zhihong, Meng Qingkui, Zhang Kaisong, Chen Limei, 2022. Analysis of High Precision Aeromagnetic Data in Liaoning and Its Adjacent Areas: Constraints on Regional Fault Zones and Lithospheric Thermal Structure. Earth Science, 47(9): 3401-3416. doi: 10.3799/dqkx.2022.131
    Citation: Gao Wei, Shu Qing, Guo Zhihong, Meng Qingkui, Zhang Kaisong, Chen Limei, 2022. Analysis of High Precision Aeromagnetic Data in Liaoning and Its Adjacent Areas: Constraints on Regional Fault Zones and Lithospheric Thermal Structure. Earth Science, 47(9): 3401-3416. doi: 10.3799/dqkx.2022.131

    Analysis of High Precision Aeromagnetic Data in Liaoning and Its Adjacent Areas: Constraints on Regional Fault Zones and Lithospheric Thermal Structure

    doi: 10.3799/dqkx.2022.131
    • Received Date: 2022-03-11
    • Publish Date: 2022-09-25
    • Analysis and mining of high-precision aeromagnetic data is one of the important methods to reveal the spatial distribution of regional deep fault zones and lithospheric thermal structure. In order to reveal the relationship between the aeromagnetic anomaly and the regional fault zones and estimate the Curie-point depths and lithospheric thicknesses in Liaoning and its adjacent areas, the Curie-point depths are calculated by the power spectrum method, based on reduction to pole of aeromagnetic data. Meanwhile, the lithospheric thicknesses of the eastern segments of Liaoning are calculated by the 1D stable thermal conduction equations. Our new aeromagnetic data reveals that: (1) There are several NE/NNE striking aeromagnetic anomaly zones in the eastern and western parts of Liaoning and the Bohai Bay, which are interpreted as the products of the alternation of long-term extension and brief compression of the active continental margins under the background of the Pacific Plate subduction since the Late Mesozoic. The near NW/NWW striking aeromagnetic anomaly zones in the northern segments of Liaoning, which are interrupted by the NE/NNE striking magnetic anomaly zones, are interpreted as the tectonic traces which were extended and uplifted to the middle crust after the closure of the Paleo-Asian Ocean during the late collisional orogeny. (2) Our aeromagnetic anomalies also show that the estimated Curie-point depths of Liaoning and its adjacent areas ranges from 16 km to 40 km, with an average depth of 28 km. The heat flow values of the Fuxin and Panjin Curie uplifted are relatively higher. However, the heat flow values of the Shenyang and Liaoyuan Curie depression are relatively lower. (3) The estimated lithospheric thicknesses of the Liaoning and its adjacent areas show spatial heterogeneity, ranging from 70 km to 150 km with an average of 100 km. The estimated lithospheric thickness of the Yingkou-Anshan area near the Tan-Lu fault zone is the thinnest with a thickness of 60-80 km. The spatial heterogeneity of regional thermal lithospheric thicknesses in the eastern segments of Liaoning and Bohai Bay most likely results from the combined effects of the spatially heterogeneous distribution of wet upwellings triggered by the subducted Pacific slab and pre-existing weak zones in the cratonic lithosphere since the Late Mesozoic.

       

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