Ze-Zhou Wang

TL;DR: In this paper, a large set of zinc (Zn) stable isotope data for continental basalts from eastern China were reported to investigate the application of Zn isotopes as a new tracer of deep carbonate cycling.

TL;DR: For example, Doucet et al. as discussed by the authors reported high-precision (±0.04) Zn isotope data for well-characterized peridotites from cratonic and orogenic settings, as well as their mineral separates.

TL;DR: In this article, a series of unaltered to strongly altered oceanic peridotites were analyzed by analyzing their adsorption by ubiquitous secondary phases (e.g. goethite).

TL;DR: Wang et al. as mentioned in this paper proposed a state key laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China 2State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjinjing 210093, China 3Chinese Academy of Sciences Key Laboratory of Crust-Mantle Materials and Environments, University of Science and Technology of China, Hefei, Anhui 230026, China

TL;DR: In this article, major trace elements, Sr and Mg isotope data for thirty deep-seated mafic xenoliths, which sampled different lithospheric depths in the southeastern North China Craton (NCC), were reported.