What is it about?
The early Palaeozoic orogeny was a result of collision of the west Cathaysia domain with a postulated continent (instead of the east Cathaysia domain).
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Why is it important?
Our results show that the early Palaeozoic orogeny probably is a continental-continental orogen instead of intra-continental orogen
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This page is a summary of: Zircon U–Pb ages and Hf isotope compositions of the Chencai migmatite, central Zhejiang Province, South China: constraints on the early Palaeozoic orogeny, Geological Magazine, April 2017, Cambridge University Press,
DOI: 10.1017/s0016756817000292.
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