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Published in 2017 at "Journal of Asian Earth Sciences"
DOI: 10.1016/j.jseaes.2017.07.018
Abstract: Abstract The Late Neoproterozoic Dahongliutan BIF is associated with siliciclastic rocks in the Tianshuihai terrane of the Western Kunlun orogenic belt (WKO), NW China. The sedimentary rocks have various weathering indices (e.g., CIA = 57–87, PIA = 61–96 and…
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Keywords:
siliciclastic rocks;
neoproterozoic dahongliutan;
dahongliutan bif;
kunlun orogenic ... See more keywords