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- W2364014248 abstract "In this paper,based on the geomagnetic survey line from LuAn to YingShan in the Eastern Dabie Orogen,the geomagnetic anomaly are picked up.Assisted by the geology and seismology results,the depth of Curie surface was inverted,and the model of subsurface magnetic structure was built.According to analyzing the curve of the magnetic anomaly and magnetic structure model,it was found that the results reflect strongly the differences among the Hefei Basin,North Huaiyang area,and Eastern Dabie Orogen.In the Eastern Dabie Orogen,the magnetic structure is complex,related to the strong and undulate geomagnetic curve.In the North Huaiyang area,it shows that the geomagnetic structure is imbricate with the weak magnetic anomalies curve.And in the Hefei Basin,the basement appears deeply buried,continuous and uniform,leading to the flat magnetic anomalies curve.Simultaneously,a significant difference of magnetic properties in the area from 6 to 12 km depth in the Huoshan region is noticed.Combined with the earthquake from 1970 and strong historical earthquake,the connection of the seismicity of HuoShan seismic window with the underground structure and field resource is studied,and the dynamic causes of HouShan seismic window is discussed preliminarily." @default.
- W2364014248 created "2016-06-24" @default.
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- W2364014248 date "2013-01-01" @default.
- W2364014248 modified "2023-09-23" @default.
- W2364014248 title "The surveying of LuAn-YingShan geomagnetic profile and earthquake research in eastern Dabie orogen" @default.
- W2364014248 hasPublicationYear "2013" @default.
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