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Article Navigation >  Acta Sedimentologica Sinica  > 1983  >  1(2): 73-83

Wang Yinghua, Yang Chengyun, Zhang Xiulian. RELATIONSHIP BETWEEN THE CHANGES OF OOIDAL TEXTURE AND THE PROPERTY AND STRENGTH OF DIAGENESIS[J]. Acta Sedimentologica Sinica, 1983, 1(2): 73-83.
Citation: Wang Yinghua, Yang Chengyun, Zhang Xiulian. RELATIONSHIP BETWEEN THE CHANGES OF OOIDAL TEXTURE AND THE PROPERTY AND STRENGTH OF DIAGENESIS[J]. Acta Sedimentologica Sinica, 1983, 1(2): 73-83.
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RELATIONSHIP BETWEEN THE CHANGES OF OOIDAL TEXTURE AND THE PROPERTY AND STRENGTH OF DIAGENESIS

  • Department of Geology, Peking University

  • Received Date: 1982-05-16
  • Publish Date: 1983-06-10
  • Oolites are common grains in carbonatites, and their tenure changes arc important indicators in studying the property- and strength of diagenesis.It has been found that splits and deformed oolites formed under compaction, and the sutured tcature and the pressure shadow as }s-ell as recrystallization and dolo- mitiz anon formed under pressure solution are related to the property and st- rength of diagenesis.
  • [1] (1)王英华等,(1982)缅粒与沉积环境，地质科学论文集(第一集)，北京大学出版社。

    (2)王嘉荫，(1978)应力矿物概论，地质出版社。

    (3)罗宾·巴瑟斯特，(1971)碳酸盐沉积物及其成岩作用，中国科学院地质研究所译，科学出版社(1977)。

    (4)威尔逊，(1975)地质历史中的碳酸盐相，冯增昭等译，科学出版社(1981).

    (5)Carozzi, A.V.，(1975)Sedimentary Rocks. Copyright by Dowden, Hutch-inson and Ross, Inc.p 248-288

    (6)Blatt, H., Middleton, G.and Murray, r.，(1972)Origin of Sedimentary Rocks.Prentice-HaII, Inc.，Englewood Cliffs, New Jersey

    (7)Park, W.C.and Schot, E.H.，(1968)Stylolites; Their Nature and Origin， Jour. Sedim. Petrol. V. 38.

    (8)Carozzi, A.V.，(1960)Microscopic Sedimentary Petrography.Copyright byJohn and Sons, Inc.
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  • Received:  1982-05-16
  • Published:  1983-06-10

RELATIONSHIP BETWEEN THE CHANGES OF OOIDAL TEXTURE AND THE PROPERTY AND STRENGTH OF DIAGENESIS

  • Department of Geology, Peking University
  • Received Date: 1982-05-16
  • Publish Date: 1983-06-10

Abstract: Oolites are common grains in carbonatites, and their tenure changes arc important indicators in studying the property- and strength of diagenesis.It has been found that splits and deformed oolites formed under compaction, and the sutured tcature and the pressure shadow as }s-ell as recrystallization and dolo- mitiz anon formed under pressure solution are related to the property and st- rength of diagenesis.

Wang Yinghua, Yang Chengyun, Zhang Xiulian. RELATIONSHIP BETWEEN THE CHANGES OF OOIDAL TEXTURE AND THE PROPERTY AND STRENGTH OF DIAGENESIS[J]. Acta Sedimentologica Sinica, 1983, 1(2): 73-83.
Citation: Wang Yinghua, Yang Chengyun, Zhang Xiulian. RELATIONSHIP BETWEEN THE CHANGES OF OOIDAL TEXTURE AND THE PROPERTY AND STRENGTH OF DIAGENESIS[J]. Acta Sedimentologica Sinica, 1983, 1(2): 73-83.
shu

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