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Jiang Zhongxin. THE EMPIRICAL RELATIONS BETWEEN MD AND σ COEFFICIENT OF SANDS AND THEIR REFLECTION ON THE DEPOSITIONAL ENVIRONMENT[J]. Acta Sedimentologica Sinica, 1985, 3(1): 128-137.
Citation: Jiang Zhongxin. THE EMPIRICAL RELATIONS BETWEEN MD AND σ COEFFICIENT OF SANDS AND THEIR REFLECTION ON THE DEPOSITIONAL ENVIRONMENT[J]. Acta Sedimentologica Sinica, 1985, 3(1): 128-137.

THE EMPIRICAL RELATIONS BETWEEN MD AND σ COEFFICIENT OF SANDS AND THEIR REFLECTION ON THE DEPOSITIONAL ENVIRONMENT

  • Received Date: 1983-06-22
  • Publish Date: 1985-03-10
  • The size analysis of sands in the littoral area of Qinhuangdao shows that the empircal relationships between median diameter, Md, and sorting coefficient,σ, of sands different types and characteristics due to various geneses and hydrodynamic conditions.Therefore,they may be attributed to different depositional environments. A linear σ-Md graph with ascending grade suggests that the sorting of sand particles becomes better as they run way in removal and grow smaller in size, which implies a normal state of depositional differentiation.And down-sloped σ-Md line indicates that when sand particles grow smaller in transportation, their sorting becomes poorer. This means an abnormal depositional differentiation by the disturbance of wash
  • [1] (1)鲁欣,1953,沉积岩石学原理,中册,地质出版社(1955)。

    (2)成都地质学院陕北队,1978,沉积岩(物)粒度分析及其应用,地质出版社。

    (3)宋天锐、梁百合,1978,我国南方的两种现代滨海沉积类型,地质学报,52卷2期。

    (4)埃默里,K, O.1961,中国东海和南海浅海部分的沉积,海洋译丛,1965年1期。

    (5)埃默里,K, O. 1968,世界大陆架上的残留沉积,海洋地质参考资料,1975年2期。
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  • Received:  1983-06-22
  • Published:  1985-03-10

THE EMPIRICAL RELATIONS BETWEEN MD AND σ COEFFICIENT OF SANDS AND THEIR REFLECTION ON THE DEPOSITIONAL ENVIRONMENT

Abstract: The size analysis of sands in the littoral area of Qinhuangdao shows that the empircal relationships between median diameter, Md, and sorting coefficient,σ, of sands different types and characteristics due to various geneses and hydrodynamic conditions.Therefore,they may be attributed to different depositional environments. A linear σ-Md graph with ascending grade suggests that the sorting of sand particles becomes better as they run way in removal and grow smaller in size, which implies a normal state of depositional differentiation.And down-sloped σ-Md line indicates that when sand particles grow smaller in transportation, their sorting becomes poorer. This means an abnormal depositional differentiation by the disturbance of wash

Jiang Zhongxin. THE EMPIRICAL RELATIONS BETWEEN MD AND σ COEFFICIENT OF SANDS AND THEIR REFLECTION ON THE DEPOSITIONAL ENVIRONMENT[J]. Acta Sedimentologica Sinica, 1985, 3(1): 128-137.
Citation: Jiang Zhongxin. THE EMPIRICAL RELATIONS BETWEEN MD AND σ COEFFICIENT OF SANDS AND THEIR REFLECTION ON THE DEPOSITIONAL ENVIRONMENT[J]. Acta Sedimentologica Sinica, 1985, 3(1): 128-137.
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