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- W2365651503 abstract "In this paper, the data from deep seismic reflection and wide angle reflection profiling completed in the Sanhe-Pinggu great earthquake (M=8.0) area are comprehensively studied and interpreted. The results shows that the layered crustal structures obtained by the two investigation methods are basically consistent. In the Sanhe-Pinggu earthquake area, where the fluctuation and variation of basement structures are conside- rable and shallow faults well developed, the thickness of the upper crust and the depth of Moho interface are 21～23km and 36～37km, respectively. Among several fault zones determined by this study, the Xiadian fault is a tectonic zone with obvious characteristics and coexistence of both shallow and deep faults. Surrounding the focus, anomalous velocity structures which exhibit apparent differences along with special and complex geological tectonic environment mean that these parts are favorable for earthquake occurrence. The phenomena of Moho interface fluctuation and rather thick overlapping reflection layers and existence of locally complex cuneiform reflection zones and so on, indicate that the strong compression and deformation of the crustal structures had taken place in this region, and magmatic activity caused strong reformation of materials and structures in lower crust, further more resulted in complicated deep crustal structures in the area and maybe regarded as the deep background for the development and occurrence of Sanhe-Pinggu M8 earthquake." @default.
- W2365651503 created "2016-06-24" @default.
- W2365651503 creator A5036746989 @default.
- W2365651503 date "2004-01-01" @default.
- W2365651503 modified "2023-09-25" @default.
- W2365651503 title "DEEP STRUCTURAL FEATURES OF THE SANHE-PINGGU GREAT EARTHQUAKE AREA IMAGED BY WIDE-ANGLE AND DEEP SEISMIC REFLECTION PROFILING" @default.
- W2365651503 hasPublicationYear "2004" @default.
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