Contributions to Sequence Stratigraphy from the Quaternary Studies in Japan

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Studies of sequence stratigraphy in Japan began in the early 1990s with the Quaternary successions, especially the Plio-Pleistocene of the southern Kanto area. Comprehensive geologic researches in this area provided a framework for the application of the sequence-stratigraphic principles to the onshore outcrops. The outcome of such studies represents one type of variation in the standard sequence-stratigraphic model. In particular, such studies have clarified some kinds of variations in the sequence-stratigraphic tenet. That is (1) diachroneity of systems tracts, (2) spatial and temporal relationship between high-frequency depositional sequences and parasequences, (3) relative timing of turbidite deposition in a submarine fan environment, and (4) contemporaneity of lowstand depositional systems. Furthermore, sequence-stratigraphic classification of the Quaternary successions, together with tentative correlation of sequence boundaries with the oxygen isotopic sea-level index, permits detailed chronostratigraphic correlation of such successions developed in the Osaka and Boso areas. Recently, detailed measurements of depositional rates in a Holocene sequence has been available. Such measurements identified several different patterns of depositional rates that characterize each of a wide range of shallow marine and coastal depositional systems.

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  • 第四紀研究  

    第四紀研究 38(3), 184-193, 1999-06-01 

    Japan Association for Quaternary Research

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各種コード

  • NII論文ID(NAID)
    10002511307
  • NII書誌ID(NCID)
    AN0034136X
  • 本文言語コード
    ENG
  • 資料種別
    REV
  • ISSN
    04182642
  • NDL 記事登録ID
    4749600
  • NDL 雑誌分類
    ZM49(科学技術--地球科学--地質)
  • NDL 請求記号
    Z15-67
  • データ提供元
    CJP書誌  CJP引用  NDL  J-STAGE 
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