Oceanic lithospheric mantle beneath the continental crust of the Chinese Altai Chao Yuan Min Sun Yigang Xu Guochun Zhao Wenjiao Xiao Xiaoping Long Jiyuan Yin 10.6084/m9.figshare.3452849 https://geolsoc.figshare.com/articles/dataset/Oceanic_lithospheric_mantle_beneath_the_continental_crust_of_the_Chinese_Altai/3452849 <p>Although subduction–accretion is proposed as a major regime in making new continental crust, how the lithospheric mantle forms remains unclear. Formed after the closure of the Palaeo-Asian Ocean, the Ashele basalt shows normal mid-ocean ridge basalt (N-MORB)-like characteristics with light REE-depleted patterns and extremely low contents of high field strength elements. The low Zr/Y and Nb/Y ratios of the basalt are significantly different from those of asthenosphere-derived melts, and the excess Eu and Sr suggest that the basalt was probably derived from accreted oceanic lithospheric mantle. The presence of the N-MORB-like terrestrial basalt implies that subduction–accretion is an effective mechanism in building the refractory lithospheric mantle of Phanerozoic continents. </p> 2016-06-21 10:21:50 lithospheric mantle lithospheric mantle forms crust Chinese Altai field strength elements Ashele basalt Phanerozoic continents Oceanic lithospheric mantle subduction oceanic lithospheric mantle Geology