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Article Navigation >  Acta Sedimentologica Sinica  > 1996  >  14(S1): 75-83

He Haiqin. Depositional Microfacies,Cycles,Sedimentary Environment and Evolution of the Qixia Formation in Zhejiang Province,China[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 75-83.
Citation: He Haiqin. Depositional Microfacies,Cycles,Sedimentary Environment and Evolution of the Qixia Formation in Zhejiang Province,China[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 75-83.
shu

Depositional Microfacies,Cycles,Sedimentary Environment and Evolution of the Qixia Formation in Zhejiang Province,China

  • Research Institute of Petroleum Exploration and Development,CNPC,Beijing 100083

  • Received Date: 1996-01-12
  • Publish Date: 1996-12-31
  • Based on the sedimentary microfactes and bioecologic analysis of the Qixia formation of three sections in studied area, this paper summaries the depositional rhythms, cycles and sedimentary environment of the Qixia formation, and further analyses the characteristics of its sedimentary evolution. The results suggest that the Qixia formation was formed in a subtidal,low energy, open and non-barrier carbonate ramp belt.
  • [1] 1.沙庆安，吴望始，傅家澳主编.拼桂地区二.系综合研究一兼论含油气性.北京:科学出版社，1990.

    2.冯增昭等.中下扬子地区二.纪岩相古地理.北京:地质出版社，1991, 244.

    3.吕炳泉等.下扬子地区早二.世海进和上升流形成的块级环境沉积.科学通报，1989. 34 (22):1721-1724.

    4. Ahr W M. The Carbonate Ramp: an Alternative to the Shelf Model. Trans, Gulf Coast Assoc, Gaol.Soc. 1973. 23: 221-225.
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Publishing history
  • Received:  1996-01-12
  • Published:  1996-12-31

Depositional Microfacies,Cycles,Sedimentary Environment and Evolution of the Qixia Formation in Zhejiang Province,China

  • Research Institute of Petroleum Exploration and Development,CNPC,Beijing 100083
  • Received Date: 1996-01-12
  • Publish Date: 1996-12-31

Abstract: Based on the sedimentary microfactes and bioecologic analysis of the Qixia formation of three sections in studied area, this paper summaries the depositional rhythms, cycles and sedimentary environment of the Qixia formation, and further analyses the characteristics of its sedimentary evolution. The results suggest that the Qixia formation was formed in a subtidal,low energy, open and non-barrier carbonate ramp belt.

He Haiqin. Depositional Microfacies,Cycles,Sedimentary Environment and Evolution of the Qixia Formation in Zhejiang Province,China[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 75-83.
Citation: He Haiqin. Depositional Microfacies,Cycles,Sedimentary Environment and Evolution of the Qixia Formation in Zhejiang Province,China[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 75-83.
shu

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