SEDIMENTARY CHARACTERISTICS OF CARBONATE GRAIVTY FLOWS ON THE CONTINENTAL SLOPE OF THE EARLY TRIASSIC IN SOUTHERN GUIZHOU AND WESTERN GUANGXI

Wang Yigang

ISSN 1000-0550 CN 62-1038/P

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Article Navigation > Acta Sedimentologica Sinica > 1986 > 4(2): 91-100

Wang Yigang. SEDIMENTARY CHARACTERISTICS OF CARBONATE GRAIVTY FLOWS ON THE CONTINENTAL SLOPE OF THE EARLY TRIASSIC IN SOUTHERN GUIZHOU AND WESTERN GUANGXI[J]. Acta Sedimentologica Sinica, 1986, 4(2): 91-100.

Citation:

Wang Yigang. SEDIMENTARY CHARACTERISTICS OF CARBONATE GRAIVTY FLOWS ON THE CONTINENTAL SLOPE OF THE EARLY TRIASSIC IN SOUTHERN GUIZHOU AND WESTERN GUANGXI[J]. Acta Sedimentologica Sinica, 1986, 4(2): 91-100.

SEDIMENTARY CHARACTERISTICS OF CARBONATE GRAIVTY FLOWS ON THE CONTINENTAL SLOPE OF THE EARLY TRIASSIC IN SOUTHERN GUIZHOU AND WESTERN GUANGXI

Wang Yigang

Research Institute of Sichuan Petroleum Geological Exploration and Development

Received Date: 1984-06-21
Publish Date: 1986-06-10

Abstract

In Early Triassic sea area in Southern Guizhou and Western Guangxi，there exis- ted a carbonate sedimentary pattern of continental slope without bioherm,which was about 400 km long，25-70 km wide and roughly speard with a "S" pattern from nor- th-east to south-west.

References

[1]	王一刚，1984年，石油实验地质，第6卷，第1期，18-23页。
[2]	约翰逊" A " H, 1970，张之立等译，1983，地质学中的物理过程，科学出版社。 [3)赖内克H"E，辛格·I " B, 1979，陈昌明等译，陆源碎屑沉积环境，石油工业出版社。
[3]	Middleton, G" V" and Hamnton, M, A"，1973, Turbidites and Deep Water Sedimentation, 1-38, SEMP Pacific Section Short Course.

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通讯作者: 陈斌, bchen63@163.com

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沈阳化工大学材料科学与工程学院沈阳 110142

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