岡山平野の泥炭層から推測される完新世の海水準変動と古環境変遷  [in Japanese]

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Author(s)

Abstract

Quaternary peat beds from bore-hole samples deliver information to reconstruct paleoenvironment. Altitudes ofdated non-marine peat beds and marine beds allow to be created a sea-level curve. 4 peat beds (A to D) areidentified from the uppermost Pleistocene to Holocene deposits of the Okayama Plain. They thought to bedeposited at stable events during sea-level change.

Journal

  • Okayama University Earth Science Report

    Okayama University Earth Science Report 19(1), 1-4, 2012-12-26

    岡山大学理学部地球科学教室

Codes

  • NII Article ID (NAID)
    120005232325
  • NII NACSIS-CAT ID (NCID)
    AN10506284
  • Text Lang
    JPN
  • Article Type
    departmental bulletin paper
  • ISSN
    1340-7414
  • Data Source
    IR 
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