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The Sulu ultra-high pressure(UHP)metamorphic belt in Eastern China is well known as the eastern extension of the Qingling-Dabie orogenic belt formed by subduction and collision between the Sino-Korean and Yangtze cratons.The main hole of the Chinese Continental Scientific Drilling(CCSD)project is located at the southern segment of the Sulu UHP metamorphic belt(34°25′N/118°40′E),about 17 km southwest of Donghai County.Integrated geophysical investigations using gravity,magnetic,deep seismic
The Sulu ultra-high pressure (UHP) metamorphic belt in Eastern China is well known as the eastern extension of the Qingling-Dabie orogenic belt formed by subduction and collision between the Sino-Korean and Yangtze cratons. The main hole of the Chinese Continental Scientific Drilling (CCSD) project is located at the southern segment of the Sulu UHP metamorphic belt (34 ° 25’N / 118 ° 40’E), about 17 km southwest of Donghai County. Templated geophysical investigations using gravity, magnetic, deep seismic