Yongzhang Zhou

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Mingguo Zhai1
Panagiotis Ch. Voudouris1
1Mingguo Zhai
1Panagiotis Ch. Voudouris
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Marine siliceous rocks are widely distributed in the central orogenic belt (COB) of China and have a close connection to the geological evolution and metallogenesis. They display periodic distributions from Mesoproterozoic to Jurassic with positive peaks in the Mesoproterozoic, Cambrian--Ordovician, and Carboniferous--Permian and their deposition is(More)
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