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Article Navigation >  Acta Sedimentologica Sinica  > 1999  >  17(1): 30-37

Zhao Guolian. The Influence of Biogenic Procession on the Accumulation and Precipiation of Silica—An example from South of Anhui and West of Zhejiang[J]. Acta Sedimentologica Sinica, 1999, 17(1): 30-37.
Citation: Zhao Guolian. The Influence of Biogenic Procession on the Accumulation and Precipiation of Silica—An example from South of Anhui and West of Zhejiang[J]. Acta Sedimentologica Sinica, 1999, 17(1): 30-37.
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The Influence of Biogenic Procession on the Accumulation and Precipiation of Silica—An example from South of Anhui and West of Zhejiang

  • Institute of Geophysics,Chinese Academy Sciences Beijing 100101

  • Received Date: 1998-03-04
  • Rev Recd Date: 1998-04-30
  • Publish Date: 1999-03-10
  • In the South of Anhui and West of Zhejiang, there is a zo ne of upper Sinian and low er Cambrian siliceous rocks w hich strech strch praximately NE.Af ter field t rip and labo ratory studies,We understood all aspects of thier tex ture and structure and mineral composi tio n and found shell of radiolarian.It is proved that biogenic procession plays an important role in the fomat ion of chert s of chert s and the analy sis of major elements shows it clearly.
  • [1] 1 王东安.扬子地台晚元古代以来硅岩地球化学特征及其成因.地质科学, 1994, 29(1):41～54

    2 谢窦克.皖南浙西上震旦统碧玉岩的地质意义.中国地质科学院南京地质矿产研究所刊, 1979

    3 Brassell S C. Applicat ions of bi omarkers for delineating marine paleoclimatic flutuat ions during the Pleistocene.In :Engel M H, Macko S A, eds Organic Geochemi stry Principles and Applications.Plenum Press, 1993.699～738

    4 Fu Jiamo, S heng Guoying, Xu Jiayou, Eglinton G, Gow ar A P, Jia Rongfen, Fan Shanf a, Peng Pingan.Application of biological markersin the assessment of paleoenvi ronment s of Chinese non -marine sediments.Org.Geochem, 1990, 16 :769～770
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Publishing history
  • Received:  1998-03-04
  • Revised:  1998-04-30
  • Published:  1999-03-10

The Influence of Biogenic Procession on the Accumulation and Precipiation of Silica—An example from South of Anhui and West of Zhejiang

  • Institute of Geophysics,Chinese Academy Sciences Beijing 100101
  • Received Date: 1998-03-04
  • Rev Recd Date: 1998-04-30
  • Publish Date: 1999-03-10

Abstract: In the South of Anhui and West of Zhejiang, there is a zo ne of upper Sinian and low er Cambrian siliceous rocks w hich strech strch praximately NE.Af ter field t rip and labo ratory studies,We understood all aspects of thier tex ture and structure and mineral composi tio n and found shell of radiolarian.It is proved that biogenic procession plays an important role in the fomat ion of chert s of chert s and the analy sis of major elements shows it clearly.

Zhao Guolian. The Influence of Biogenic Procession on the Accumulation and Precipiation of Silica—An example from South of Anhui and West of Zhejiang[J]. Acta Sedimentologica Sinica, 1999, 17(1): 30-37.
Citation: Zhao Guolian. The Influence of Biogenic Procession on the Accumulation and Precipiation of Silica—An example from South of Anhui and West of Zhejiang[J]. Acta Sedimentologica Sinica, 1999, 17(1): 30-37.
shu

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