The reefs widely developed from Sinian to Neogene in China, with main reef-forming stages in Devonian, Permian and Neogene, respectively.

  • 摘要中国生物礁从震旦纪至新近纪均有发育,分布范围广,并有泥盆纪、二叠纪和新近纪3个主要造礁期。
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