Article ID Journal Published Year Pages File Type
6443794 Journal of African Earth Sciences 2014 9 Pages PDF
Abstract
The homogeneity of the Pb isotopes in the studied kaolin deposits indicates that the Pb isotopes cannot be used as tracer for source area composition of kaolin deposits, while the systematic variations of both Sr and Nd isotopes among the studied deposits suggest their possible use to differentiate between sedimentary kaolin deposits based on their source rock compositions.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
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