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The North China Craton (NCC) and Central Asian Orogen Belt (CAOB) in Northeastern China experienced a range of tectonic events during the Phanerozoic, dominated by lithospheric thinning of the eastern NCC in the late Mesozoic and Cenozoic. In order to better understand the tectonic evolution of the NCC and the CAOB, new broadband and long period magnetotelluric data were collected along a north-west...
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