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    Volume 33 Issue 5
    Sep.  2008
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    Article Contents
    MA Hong-sheng, ZHANG Guo-min, WEN Xue-ze, ZHOU Long-quan, SHAO Zhi-gang, 2008. 3-D P Wave Velocity Structure Tomographic Inversion and Its Tectonic Interpretation in Southwest China. Earth Science, 33(5): 591-602.
    Citation: MA Hong-sheng, ZHANG Guo-min, WEN Xue-ze, ZHOU Long-quan, SHAO Zhi-gang, 2008. 3-D P Wave Velocity Structure Tomographic Inversion and Its Tectonic Interpretation in Southwest China. Earth Science, 33(5): 591-602.

    3-D P Wave Velocity Structure Tomographic Inversion and Its Tectonic Interpretation in Southwest China

    • Received Date: 2008-05-10
    • Publish Date: 2008-09-25
    • We have selected about 60000 arrival times recorded by 205 regional stations, with the seismic tomography theory and three dimensional ray tracing method, to determine a detailed three-dimensional (3-D) P wave velocity structure of the lithosphere in southwest China. Then we present the medium structure and tectonic characteristics of different depth which are reflected by the 3-D P wave velocity image in this area, integrated with the previous geological features and geophysical data. The results suggest that deposit basins and alpine mountainous regions present as negative anomaly, with some montage negative anomalies even extending to the deep crust or the upper mantle, which reflects the sharp rising of the new orogens and the concomitant gravity equilibrium; low-velocity layers exist far and wide in the middle and deep crust under the large fault zones around the Sichuan-Yunnan block, which can be taken as the decoupling layer adjusting the faults and blocks movement; some deep structures related with the main active faults, and the trends and extending depths can be distinguished from the P wave velocity image.

       

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