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Su Dechen, Mei Mingxiang. Discussion on Some Problems Relating to Sedimentology and Stratigraphy[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 33-37.
Citation: Su Dechen, Mei Mingxiang. Discussion on Some Problems Relating to Sedimentology and Stratigraphy[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 33-37.

Discussion on Some Problems Relating to Sedimentology and Stratigraphy

  • Received Date: 1995-08-03
  • Publish Date: 1996-12-31
  • Relations between sedimentology and stratigraphy, sedimentology and sequence stratigraphy, sequence stratigraphy and cyclostratigraphy are discussed with the principles of sedimentology being highly emphasized. Four types of equence boundaries are recognized. Hence, a sequence is defined as a series of genetically closely related sedimentary rocks formed in a longterm (third-or forth-order) transgrassive-regrassive cycle. Any rock surface between two different lithofacies which represent two slow long-term different transgrassive-regrassive cycles can be regarded as the sequence boundary. Sequence, stratigraphy, cyclostratigraphy, lithostratigraphy, biostratigraphy and etc. must be crossreferred.
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    3.吴瑞棠,王治平.地层学原理及方法.地质出版社,1994.

    4.Goldhammer R K, Ixhmann P J, Dunn P J. The origin of high-frequency platform carbonate cycles and third-order se-quences: constraints from outcrop data and stratigraphic modeling. Journal of Sedimentary Petrology. 1993. 63 (3):318-359.

    5.CK威尔格斯等编,徐怀大等译.层序地层学原理.北京:石油工业出版社,1993.

    6.许效松等.层序地层学研究进展.岩相古地理,1994. 14 (1) : 34-39.

    7.Goodwin P W and Anderson E J. Punctuated aggradational cycles:a general hypothesis of episodic stratigraphic accu-mutation. Journal of Geology. 1985. 93: 515-533.

    8.Einsele. et al. Cyclic and Event Stratification. Springer. 1982.

    9.Einsele, et al. Cycles and events in stratifraphy. Springer. 1991.

    10.Li Y Y &Perlmutter M A. Global cyclostratigraphy: a model of carbonate growth patterns. Marine and Petroleum.1993. 10.
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  • Received:  1995-08-03
  • Published:  1996-12-31

Discussion on Some Problems Relating to Sedimentology and Stratigraphy

Abstract: Relations between sedimentology and stratigraphy, sedimentology and sequence stratigraphy, sequence stratigraphy and cyclostratigraphy are discussed with the principles of sedimentology being highly emphasized. Four types of equence boundaries are recognized. Hence, a sequence is defined as a series of genetically closely related sedimentary rocks formed in a longterm (third-or forth-order) transgrassive-regrassive cycle. Any rock surface between two different lithofacies which represent two slow long-term different transgrassive-regrassive cycles can be regarded as the sequence boundary. Sequence, stratigraphy, cyclostratigraphy, lithostratigraphy, biostratigraphy and etc. must be crossreferred.

Su Dechen, Mei Mingxiang. Discussion on Some Problems Relating to Sedimentology and Stratigraphy[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 33-37.
Citation: Su Dechen, Mei Mingxiang. Discussion on Some Problems Relating to Sedimentology and Stratigraphy[J]. Acta Sedimentologica Sinica, 1996, 14(S1): 33-37.
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