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Fang Shaoxian, Hou Fanghao. THE CARBONIFEROUS SEDIMENTARY ENVIRONMENTS AND THE BRYOZOAN-CORAL PATCH REEF OF THE DA-TANG AGE OF THE LONG-PING CARBONATE PLATFORM IN TIANLING COUNTY,GUANGXI PROVINCE[J]. Acta Sedimentologica Sinica, 1986, 4(3): 30-42.
Citation: Fang Shaoxian, Hou Fanghao. THE CARBONIFEROUS SEDIMENTARY ENVIRONMENTS AND THE BRYOZOAN-CORAL PATCH REEF OF THE DA-TANG AGE OF THE LONG-PING CARBONATE PLATFORM IN TIANLING COUNTY,GUANGXI PROVINCE[J]. Acta Sedimentologica Sinica, 1986, 4(3): 30-42.

THE CARBONIFEROUS SEDIMENTARY ENVIRONMENTS AND THE BRYOZOAN-CORAL PATCH REEF OF THE DA-TANG AGE OF THE LONG-PING CARBONATE PLATFORM IN TIANLING COUNTY,GUANGXI PROVINCE

  • Received Date: 1984-10-17
  • Publish Date: 1986-09-10
  • The Longping carbonate platform is located in the N anpan River area in the w estern part of the continental m argin fault basin in South China. In this area, it is a smaller one in a series of isolated carbonate platforms. It is surrounded by the NW and NE trench-rift of the graben type. The platforms are formed by the rising of horst fault. In the Carboniferous epoch, there was a successional carbonate deposits area. T he bryozoan-coral reef is located in the southern tip of the plat- form--sear Gan Dong Zi.
  • [1] 西南石油学院碳酸盐岩研究室,1982,西南石油学院学报,第1期,1 -15页。
    [2] G.v.奇林格等主编,196?,碳酸盐岩(沉积学进度9A,9B),石油化学工业出版社,冯增昭等译。
    [3] J.L.威尔逊等,1975,地质历史中的碳酸盐相,地质出版社。
    [4] O .A. Jones and R.Endean, 1977, Biology and Geology of Coral rieefs,Academic Press, Ne}" York, San Fancisco, London, P.1-53.
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  • Received:  1984-10-17
  • Published:  1986-09-10

THE CARBONIFEROUS SEDIMENTARY ENVIRONMENTS AND THE BRYOZOAN-CORAL PATCH REEF OF THE DA-TANG AGE OF THE LONG-PING CARBONATE PLATFORM IN TIANLING COUNTY,GUANGXI PROVINCE

Abstract: The Longping carbonate platform is located in the N anpan River area in the w estern part of the continental m argin fault basin in South China. In this area, it is a smaller one in a series of isolated carbonate platforms. It is surrounded by the NW and NE trench-rift of the graben type. The platforms are formed by the rising of horst fault. In the Carboniferous epoch, there was a successional carbonate deposits area. T he bryozoan-coral reef is located in the southern tip of the plat- form--sear Gan Dong Zi.

Fang Shaoxian, Hou Fanghao. THE CARBONIFEROUS SEDIMENTARY ENVIRONMENTS AND THE BRYOZOAN-CORAL PATCH REEF OF THE DA-TANG AGE OF THE LONG-PING CARBONATE PLATFORM IN TIANLING COUNTY,GUANGXI PROVINCE[J]. Acta Sedimentologica Sinica, 1986, 4(3): 30-42.
Citation: Fang Shaoxian, Hou Fanghao. THE CARBONIFEROUS SEDIMENTARY ENVIRONMENTS AND THE BRYOZOAN-CORAL PATCH REEF OF THE DA-TANG AGE OF THE LONG-PING CARBONATE PLATFORM IN TIANLING COUNTY,GUANGXI PROVINCE[J]. Acta Sedimentologica Sinica, 1986, 4(3): 30-42.
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