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《Chinese Journal of Geophysics》 2008-01
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Crustal S-wave Q estimated from M_L amplitude Ⅱ:Q lateral variation in China

WANG Su-Yun~1,PEI Shun-Ping~2,Thomas M. Hearn~3,XU Zhong-Huai~1,James F. Ni~3,YU Yan-Xiang~11 Institute of Geophysics, China Earthquake Administration, Beijing 100081, China2 Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China3 New Mexico State University, Physics Department, Las Cruces, NM 88003, USA  
Over 54000 S wave amplitude and period data reported in the Annual Bulletin of Chinese Earthquakes (1984-2004) for M_L determination were used to study the S wave attenuation and the regional variation of crustal attenuation in China. A two-dimensional tomography method is adopted to find regional attenuation variation. We obtained an average Q_0 (Q at 1 Hz) value of 370 for the entire studied region with regional fluctuations ±200. Features larger than 2 degrees in most parts of China are well resolved and map directly to geologic provinces. Regions with the lowest attenuation (high Q_0 values) are beneath the Tarim Basin, Sichuan Basin, Ordos Platform, and South China Block. These tend to be tectonically inactive regions that are generally dominated by intrusive and cratonic rocks in the upper crust. Regions with the highest attenuation (low Q_0 values) are beneath Bohai Basin, Sichuan-Yunnan, North China basin, and regions beneath the Tian Shan, Qilian Shan and Fenwei graben also have low Q_0 values. These are predominantly active basins and fold belts.
【Fund】: 国家自然科学基金(40674031 40374017);; 国家科技支撑计划(2006BAC13B01)
【CateGory Index】: P315.31
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