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- W2366805962 abstract "There exists boundary claystone near the boundary between both the marine and terrestrial Per-mian and Triassic in the eastern Yunnan-western Guizhou area.This paper in troduces the characteristics of the boundary terrestrial claystone in the area and discusses its origin.The principal minerals of the clay-stone are illite-montmorillonite mixed-layer minerals(20%-80%)and kaolinite(35%-80%),and the frag-ments include zircon,apatite,hexagonal dipyramidal high-temperature quartz and other types of quartz and micro spherules.It is suggested that the terrestrial boundary claystone in the area mainly formed by volcan-ism,accompanied by normal deposition and influence of impact." @default.
- W2366805962 created "2016-06-24" @default.
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- W2366805962 date "2002-01-01" @default.
- W2366805962 modified "2023-09-25" @default.
- W2366805962 title "Characteristics of claystone at the continental Permian-Triassic boundary in the eastern Yunnan-western Guizhou region" @default.
- W2366805962 hasPublicationYear "2002" @default.
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