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DONG Wenuming, SHEN Ya, ZHOU Hong-rui, CUI Xin-sheng. Application of Sequence Stratigraphy to Precambian Strata—A case study on the Sinian in Western Henan Province[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 742-746.
Citation: DONG Wenuming, SHEN Ya, ZHOU Hong-rui, CUI Xin-sheng. Application of Sequence Stratigraphy to Precambian Strata—A case study on the Sinian in Western Henan Province[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 742-746.

Application of Sequence Stratigraphy to Precambian Strata—A case study on the Sinian in Western Henan Province

  • Received Date: 1998-11-08
  • Rev Recd Date: 1999-04-27
  • Publish Date: 1999-12-10
  • The paper focuses on sequence stratigraphy of the Sinian in Western Henan Province. Based on the theory of sequence stratigraphy,three type I sequences have been identified, in which the first two sequences correlate to the Huanglianduo Formation and Dongjia Formation,respectively,and the third one includes both the Luoquan and Dongpo Formations. After establishing their sequence isochronic framework,the author analyzes systematically the distribution patterns and genetic relations of the strata and sedimentary facies zones within the framework,and then proposes that the formation of the Sinian sequences and their system tracts in the study area was controlled primarily by the relative sea-level changes. The sediments which deposited within the same sea-level changes,although they have different sedimentary environments and different components, are isochrononic and can be correlated. Finally,the author proposes a method how to drove the curves of relative sea-level changes. Based on the research result,the author concludes that the theory of sequence stratigraghy can be generally applied to the Precambian,such as the Sinian,by identifying the key boundaries,especially the sequence boundary (SB) and the maximum flooding surface (mls),and analyzing the features of the parasequences,parasequence sets and system tracts within a sequence. The method establishes a good base for the classification and correlation of the strata study. But the hierarchy of the sequence cannot be precisely determined because of low-studying-level and short of accurate dating,therefore further studies are necessary.
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    2 威尔格斯CK等编,许怀大,魏魁生,洪卫东等译.层序地层学原理[M].北京:石油工业出版社,1993

    3 崔新省,董文明,周洪瑞.豫西震旦系瑟头层序地层学初步研究及其意义[J].地球科学,1996,21(3):249-253

    4 关保德,耿午辰,戎治权等.河南省东秦岭北坡中一上元古界[M].郑州:河南科技出版社,1988

    5 王鸿祯主编.中国古地理图集CM7.北京:地图出版社,1985

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    8 Murray R W. Chemical criteria to identify the depositional environment of chert:eeneral principles and applications[J].SedimentaryGeology,1994,90:213-232

    9 张玲华.华北地台南缘震旦纪地层沉积类型及岩相古地理研究[M].北京:中国地质大学,1989.

    11 Vail P R, Mitchum R M, Todd RG,et al. Seismic Stratigraphy and global changes of sea-level. In: Payton C E,ed. Seismic stratig-raphy-application to hydrocarbon explorationCC7. AAPG Memoir,1977(26):49一212

    12 Fisher AG, Boer PL, Silua P. Cyclostratigraphy [A].In: Creta-ceous resources, events and rhvthmsCC}. 1990. 139-772
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  • Received:  1998-11-08
  • Revised:  1999-04-27
  • Published:  1999-12-10

Application of Sequence Stratigraphy to Precambian Strata—A case study on the Sinian in Western Henan Province

Abstract: The paper focuses on sequence stratigraphy of the Sinian in Western Henan Province. Based on the theory of sequence stratigraphy,three type I sequences have been identified, in which the first two sequences correlate to the Huanglianduo Formation and Dongjia Formation,respectively,and the third one includes both the Luoquan and Dongpo Formations. After establishing their sequence isochronic framework,the author analyzes systematically the distribution patterns and genetic relations of the strata and sedimentary facies zones within the framework,and then proposes that the formation of the Sinian sequences and their system tracts in the study area was controlled primarily by the relative sea-level changes. The sediments which deposited within the same sea-level changes,although they have different sedimentary environments and different components, are isochrononic and can be correlated. Finally,the author proposes a method how to drove the curves of relative sea-level changes. Based on the research result,the author concludes that the theory of sequence stratigraghy can be generally applied to the Precambian,such as the Sinian,by identifying the key boundaries,especially the sequence boundary (SB) and the maximum flooding surface (mls),and analyzing the features of the parasequences,parasequence sets and system tracts within a sequence. The method establishes a good base for the classification and correlation of the strata study. But the hierarchy of the sequence cannot be precisely determined because of low-studying-level and short of accurate dating,therefore further studies are necessary.

DONG Wenuming, SHEN Ya, ZHOU Hong-rui, CUI Xin-sheng. Application of Sequence Stratigraphy to Precambian Strata—A case study on the Sinian in Western Henan Province[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 742-746.
Citation: DONG Wenuming, SHEN Ya, ZHOU Hong-rui, CUI Xin-sheng. Application of Sequence Stratigraphy to Precambian Strata—A case study on the Sinian in Western Henan Province[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 742-746.
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