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《Journal of Geodesy and Geodynamics》 2011-01
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CRUST THICKNESS INVERSED FROM MULTI-SCALE DECOMPOSITION OF BOUGUER GRAVITY ANOMALIES IN NORTHEASTERN OF QINGHAI-TIBET PLATEAU

Wu Lixin1),Yang Mingzhi1),Zhao Weiming1),Fu Rongshan2),Zhu Liangbao2) and Shi Xingjue2)(1)Earthquake Administration of Ningxia Hui Autonomous Region,Yinchuan 7500012)University of Science and Technology of China,Hefei 230026)  
With a gravity anomalies decomposition model,and through using the wavelet function "bior3.7",the fourth order wavelet approximate components of the Bouger gravity anomalies of northeast margin of the Qinghai-Tibetan Plateau can be obtained.Furthermore,by utilizing the Bouger gravity anomalies come from the Moho and taking the information from the 6 artificial profiles as the initial control conditions,the crustal thickness of northeastern margin of the Qinghai-Tibetan Plateau is inversed,and the inversion results are analyzed and discussed according to the crustal thickness distribution features.
【CateGory Index】: P631.1
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