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LI Shaohu. Thinking of International Sequence Stratigraphy Development and LHT Sequence Stratigraphy[J]. Acta Sedimentologica Sinica, 2010, 28(4): 735-744.
Citation: LI Shaohu. Thinking of International Sequence Stratigraphy Development and LHT Sequence Stratigraphy[J]. Acta Sedimentologica Sinica, 2010, 28(4): 735-744.

Thinking of International Sequence Stratigraphy Development and LHT Sequence Stratigraphy

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  • Corresponding author: LI Shaohu
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2010-08-10
  • Based on the research development in international sequence stratigraphy, this paper puts some viewpoints forward as follows: (1) sequence of seismic stratigraphy is different from the depositional sequence of sequence stratigraphy; (2) after 1992 the transformation from threedivided to fourdivided models, the difference between marine and continental depositional sequence makes sequence stratigraphy develop complicatedly; (3) the base level curve correlative to the fourdivided model of current sequence stratigraphy is nonperiodic and is not correlative to the periodicity of shoreline trajectory; (4) this paper introduces LHT sequence stratigraphy including conceptual model, diagrammatizing rules and approach of chronsequence framework, revamped base level curve correlative to systems tracts of LHT sequence stratigraphy. This paper redefines sequence as "a relatively conformable succession of genetically related strata bounded by remnant maximum flooding surfaces (RMFS) and their correlative subaerial unconformities (CSU)".
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2010-08-10

Thinking of International Sequence Stratigraphy Development and LHT Sequence Stratigraphy

    Corresponding author: LI Shaohu

Abstract: Based on the research development in international sequence stratigraphy, this paper puts some viewpoints forward as follows: (1) sequence of seismic stratigraphy is different from the depositional sequence of sequence stratigraphy; (2) after 1992 the transformation from threedivided to fourdivided models, the difference between marine and continental depositional sequence makes sequence stratigraphy develop complicatedly; (3) the base level curve correlative to the fourdivided model of current sequence stratigraphy is nonperiodic and is not correlative to the periodicity of shoreline trajectory; (4) this paper introduces LHT sequence stratigraphy including conceptual model, diagrammatizing rules and approach of chronsequence framework, revamped base level curve correlative to systems tracts of LHT sequence stratigraphy. This paper redefines sequence as "a relatively conformable succession of genetically related strata bounded by remnant maximum flooding surfaces (RMFS) and their correlative subaerial unconformities (CSU)".

LI Shaohu. Thinking of International Sequence Stratigraphy Development and LHT Sequence Stratigraphy[J]. Acta Sedimentologica Sinica, 2010, 28(4): 735-744.
Citation: LI Shaohu. Thinking of International Sequence Stratigraphy Development and LHT Sequence Stratigraphy[J]. Acta Sedimentologica Sinica, 2010, 28(4): 735-744.

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