Carbonated sediment recycling and its contribution to lithospheric refertilization under the northern North China Craton
Foley, Stephen F.
Ducea, Mihai N.
Geng, Xianlei; Zhang, Wen; Xu, Rong; Hu, Zhaochu; Zhou, Lian; and Wang, Zaicong
Fig. 1. Simplified tectonic map of the North China Craton (modified from Zhao et al., 2001). WB =Western block, TNCO =Trans‑North China orogen, and EB= Eastern block. Blue diamonds represent the locations of the presence of high 87Sr/86Sr peridotites
in the northern North China Craton (Wang et al., 2016; Xu et al., 2003; Zhang et al., 2009, 2012). Green circles represent the locations of the previously reported high 87Sr/86Sr carbonatites in the northern North China Craton (Chen et al., 2016; Liu et al., 2015; Yan
et al., 2007). (For interpretation of the references to color in this figure legend, the reader is referred to the web version of this article.)