Advanced Search

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

More Information
  • 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)".
  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-092024-102024-112024-122025-012025-022025-032025-042025-052025-062025-072025-0800.511.522.5
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 9.8 %FULLTEXT: 9.8 %META: 77.9 %META: 77.9 %PDF: 12.3 %PDF: 12.3 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 5.2 %其他: 5.2 %其他: 2.8 %其他: 2.8 %China: 0.6 %China: 0.6 %United States: 2.8 %United States: 2.8 %[]: 0.6 %[]: 0.6 %中卫: 0.3 %中卫: 0.3 %丽水: 0.3 %丽水: 0.3 %九江: 0.3 %九江: 0.3 %克拉玛依: 0.3 %克拉玛依: 0.3 %兰州: 0.9 %兰州: 0.9 %凉山: 0.3 %凉山: 0.3 %北京: 11.3 %北京: 11.3 %南京: 0.3 %南京: 0.3 %台州: 0.6 %台州: 0.6 %大庆: 0.9 %大庆: 0.9 %天津: 0.3 %天津: 0.3 %宜春: 0.3 %宜春: 0.3 %延安: 0.3 %延安: 0.3 %张家口: 0.9 %张家口: 0.9 %成都: 1.8 %成都: 1.8 %扬州: 0.3 %扬州: 0.3 %曼谷: 0.3 %曼谷: 0.3 %朝阳: 0.3 %朝阳: 0.3 %杭州: 1.5 %杭州: 1.5 %武汉: 0.9 %武汉: 0.9 %沧州: 5.5 %沧州: 5.5 %海口: 0.6 %海口: 0.6 %深圳: 0.3 %深圳: 0.3 %温州: 0.3 %温州: 0.3 %湖州: 0.3 %湖州: 0.3 %漯河: 0.3 %漯河: 0.3 %牡丹江: 0.3 %牡丹江: 0.3 %石家庄: 0.3 %石家庄: 0.3 %纽约: 0.3 %纽约: 0.3 %绍兴: 0.3 %绍兴: 0.3 %芒廷维尤: 7.7 %芒廷维尤: 7.7 %苏州: 0.6 %苏州: 0.6 %衢州: 0.6 %衢州: 0.6 %西宁: 43.3 %西宁: 43.3 %西安: 0.3 %西安: 0.3 %贵阳: 0.3 %贵阳: 0.3 %遂宁: 0.3 %遂宁: 0.3 %郑州: 0.3 %郑州: 0.3 %重庆: 0.9 %重庆: 0.9 %锦州: 0.3 %锦州: 0.3 %长沙: 0.3 %长沙: 0.3 %青岛: 1.8 %青岛: 1.8 %其他其他ChinaUnited States[]中卫丽水九江克拉玛依兰州凉山北京南京台州大庆天津宜春延安张家口成都扬州曼谷朝阳杭州武汉沧州海口深圳温州湖州漯河牡丹江石家庄纽约绍兴芒廷维尤苏州衢州西宁西安贵阳遂宁郑州重庆锦州长沙青岛
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(2824) PDF downloads(1460) Cited by()

Proportional views
Related
Publishing history
  • 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.

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return