Confirmation of the Permian/Triassic boundary in deep-sea sedimentary rocks; earliest Triassic condonts from black carbonaceous claystone of the Ubara section in the Tamba Belt, Southwest Japan. | Zendy

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Confirmation of the Permian/Triassic boundary in deep-sea sedimentary rocks; earliest Triassic condonts from black carbonaceous claystone of the Ubara section in the Tamba Belt, Southwest Japan.

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