Paleo—Latitude Variation of Guizhou Terrain from Devonian to Cretaceous
摘要
Over 800 paleomagnetic samples were collected from 79 sample localities,ranging in age from Devonian,Carboniferous,Permian to Jurassic for paleo-latitude research on the Guizhou terrain,The area sampled covers 13 couties with an area of about 50000km^2.The paleomagnetic results obtained indicate that the Guizhou terrain was at 11.4°S in Devonian,4.5°-9.3°S in Carboniferous,2.6°-4.5°S in Permian,14.8°N in Triassic and 24.5°-26.0°N in Jurassic,In the Cretaceous period.the paleo-latitude of the area was at 22.4-23.6°N. Therefore ,a variation curve of paleo-latitude is established in this paper for the Guizhou terrain from late Devoian to Late Cretaceous time.
引用本文（GB/T 7714）
王俊达, 李华梅. Paleo—Latitude Variation of Guizhou Terrain from Devonian to Cretaceous[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 1998.
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