SEDIMENTARY FEATURES OF THE "INTRAPLATFORM TROUGH" FACIES IN THE阴IDDLE AND LATE DEVONIAN. HUNAN GUANGXI PROVINCES
- Received Date: 1982-06-05
- Publish Date: 1983-09-10
Abstract: The deeper water facies, a special type of sedim entary facies, is distrib uted in the carbonate platform with shallow water and very shallow water went of the Middle and Late Devonian, Hunan and Guangzi Provinces,environ-The deeper water facies is called intraplatform trough0 facies, which appears as a belt.
Citation: | Chen Zhiming, Yang Peiji, Pan Zhengpu, Hou Kui, Liu Guoliang. SEDIMENTARY FEATURES OF THE "INTRAPLATFORM TROUGH" FACIES IN THE阴IDDLE AND LATE DEVONIAN. HUNAN GUANGXI PROVINCES[J]. Acta Sedimentologica Sinica, 1983, 1(3): 88-97. |