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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

  • Received Date: 1984-06-21
  • Publish Date: 1986-06-10
  • 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.
  • [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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    沈阳化工大学材料科学与工程学院 沈阳 110142

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  • Received:  1984-06-21
  • Published:  1986-06-10

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

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.

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.
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