Palaeogeographic Position of the South China Plate During the Early-Middle Devonian

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Bai Zhiqiang
Bai Shunliang Department of Geology
Peking University
Beijing
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Palaeogeographic Position of the South China Plate During the Early-Middle Devonian;
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<正> In Guangxi, the Lower- Middle Devonian boundary beds yield abundant corals, brachiopods,stromatoporoids and conodonts. The former three were common in tropical and subtropical zones, while thelast occurred only round the equator. This reveals that the South China Plate in the Early-Middle Devonianwas at or near the equator, which was also supported by palaeomagnetic study giving the palaeolatitude of theGuangxi Region at the time to be 0°36′N.
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页码:19 / 26
页数:8
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[1]  
Klapper, G,, and Trojan, W.R. 1980. Brachiopod and conodont successions in the Devonian of the northern Antelope Range, central Nevada. Johnson,J. G. Geologica et Palaeontologica .