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).
Featured Image
Why is it important?
Our results show that the early Palaeozoic orogeny probably is a continental-continental orogen instead of intra-continental orogen
Perspectives
Writing this article was a great pleasure as it has co-authors with whom I have had long standing collaborations. I hope this article provide an new explanation on the early Palaeozoic orogeny.
Longming li
Read the Original
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.
You can read the full text:
Contributors
The following have contributed to this page
