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Article Navigation >  Acta Sedimentologica Sinica  > 2009  >  27(6): 1068-1075

ZOU Caineng. Genetic Mechanism and Distribution of Sandy Debris Flows in Terrestrial Lacustrine Basin[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1068-1075.
Citation: ZOU Caineng. Genetic Mechanism and Distribution of Sandy Debris Flows in Terrestrial Lacustrine Basin[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1068-1075.
shu

Genetic Mechanism and Distribution of Sandy Debris Flows in Terrestrial Lacustrine Basin

  • Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083

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  • Corresponding author: ZOU Caineng
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2009-12-10
  • The study of deep water sedimentation has developed fifty years. The misuse of term “turbidite” to deposits of deep water is common. Then the denial of Bouma sequence as the tubidite facies sequence and related fan depositional mode, the study on deepwater has undergone circle on cognition. The sandy debris theory is an innovation and negation to classical tubidity theory.The definition, experimentation, identification feature and sedimentation model were introduced in the passage. Applying the sandy debris theory to explain the reason why thick sand bodys could occur in the center of lacke in Ordos basin. By the way, the mechanism and characteristic of sand body at slope in terrestrial lacustrine basin could be revealed. The theory would be one of theoretical basis to continental exploration.
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Publishing history
  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2009-12-10

Genetic Mechanism and Distribution of Sandy Debris Flows in Terrestrial Lacustrine Basin

  • Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083
    Corresponding author: ZOU Caineng
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2009-12-10

Abstract: The study of deep water sedimentation has developed fifty years. The misuse of term “turbidite” to deposits of deep water is common. Then the denial of Bouma sequence as the tubidite facies sequence and related fan depositional mode, the study on deepwater has undergone circle on cognition. The sandy debris theory is an innovation and negation to classical tubidity theory.The definition, experimentation, identification feature and sedimentation model were introduced in the passage. Applying the sandy debris theory to explain the reason why thick sand bodys could occur in the center of lacke in Ordos basin. By the way, the mechanism and characteristic of sand body at slope in terrestrial lacustrine basin could be revealed. The theory would be one of theoretical basis to continental exploration.

ZOU Caineng. Genetic Mechanism and Distribution of Sandy Debris Flows in Terrestrial Lacustrine Basin[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1068-1075.
Citation: ZOU Caineng. Genetic Mechanism and Distribution of Sandy Debris Flows in Terrestrial Lacustrine Basin[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1068-1075.
shu

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