Title: Conodonts of Permian-Triassic boundary beds and biostratigraphic boundary
Abstract: The Permian-Triassic boundaries in South China may be strictly classified into the eventostratigraphic boundary and the biostratigraphic boundary. The basal limit of the “boundary clay”bed is known as the eventostratigraphic boundary, whereas the biostratigraphic boundary can not be defined in relation with the “mixed beds”or “transitional beds”altogether.
Publication Year: 1995
Publication Date: 1995-01-01
Language: en
Type: article
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Cited By Count: 30
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