| Citation: |
ZHANG Ji-yan, JIANG Ting-cao, LI Xiao-quan. 1992. FEATURES OF TRIASSIC TEMPESTITES IN WESTERN GUANGXI. Geological Bulletin of China, (4): 304-310+385.
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FEATURES OF TRIASSIC TEMPESTITES IN WESTERN GUANGXI
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Abstract
The Triassic tempestites which have been discovered in western Guangxi in recent years are distributed in an area of about 160×80 km. The tempestites are exposed in the lower part of the Middle Triassic, comprising about 194 layers, with a total thickness of 63 m. The tempestiites are mainly characterized by well developed hummock bedding, wave cross-bedding and scourlng-filling structures such as bowl mold and channel mold, resulting from the storm action in an opera shelf. -
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ZHANG Ji-yan, JIANG Ting-cao, LI Xiao-quan. 1992. FEATURES OF TRIASSIC TEMPESTITES IN WESTERN GUANGXI. Geological Bulletin of China, (4): 304-310+385.
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