Velocity structure of uppermost mantle beneath China continent from Pn tomography

来源 :Science in China(Series D:Earth Sciences) | 被引量 : 0次 | 上传用户:hms0741
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39473 Pn travel times are inverted to tomographically image both lateral variation and anisotropy of uppermost mantle velocities beneath China continent. The result indicates that the overall average Pn velocity of uppermost mantle in the studied region is 8.0 km/s and the regional velocity fluctuation varies from -0.30 km/s to +0.35 km/s. Pn velocities higher than 8.2 km/s are found in the regions surrounding Qingzang Plateau, such as Junggar Basin, Tarim Basin, Qaidam Basin and Sichun Basin. Pn velocities slightly lower than the average are found in western Sichuan and Yunnan, Shanxi Graben and Bohai Bay region. A Pn velocity as low as 7.8 km/s may exist in the region striding the boundary between Guangxi and Guangdong provinces. In general, Pn velocity in tectonically stable region like cratonic platform tends to be high, while that in tecton-ically active region tends to be low. The regions in compressive setting usually show higher Pn velocity, while extensional basins or grabens generally display l 39473 Pn travel times are both inverted to tomographically image both lateral variation and anisotropy of uppermost mantle velocities beneath China continent. The result indicates that the overall average Pn velocity of uppermost mantle in the studied region is 8.0 km / s and the regional velocity fluctuation varies from -0.30 km / s to +0.35 km / s. Pn velocities higher than 8.2 km / s are found in the surrounding enclosures Qingzang Plateau, such as Junggar Basin, Tarim Basin, Qaidam Basin and Sichun Basin. Pn velocities slightly lower than the average are found in western Sichuan and Yunnan, Shanxi Graben and Bohai Bay region. A Pn velocity as low as 7.8 km / s may exist in the region striding the boundary between Guangxi and Guangdong provinces. In general, Pn velocity in tectonically stable region like cratonic platform tends to be high, while that in tecton -ically active region tends to be low. The regions in compressive setting usually show higher Pn velocity, while extensional basins or grabens generally display l
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