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Three-dimensional P-wave Velocity Structure Modelling of the Middle and Lower Reaches of the Yangtze River Metallogenic Belt: Crustal Architecture and Metallogenic Implications
Affiliation:1 School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China 2 Geological Survey of Anhui Province, Hefei 230001, China;3 Chinese Deep Exploration Center (SinoProbe Center), Chinese Academy of Geological Sciences, Beijing 100037, China;4 Anhui Earthquake Agency, Hefei 230031, China
Abstract:
Keywords:3D P-wave velocity structure   double-difference seismic tomography   crust-upper mantle   Dabie Orogen   Middle and Lower Reaches of the Yangtze River Metallogenic Belt
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