陆地和海洋环境演变研究中的释光测年进展

龚革联. 陆地和海洋环境演变研究中的释光测年进展[J]. 海洋地质与第四纪地质, 2006, 26(2): 133-138.
引用本文: 龚革联. 陆地和海洋环境演变研究中的释光测年进展[J]. 海洋地质与第四纪地质, 2006, 26(2): 133-138.
GONG Ge-lian. LUMINESCENCE DATING FOR ENVIRONMENTAL EVOLUTION STUDY IN TERRESTRIAL LAND,DEEP SEA AND COASTAL BELTS: A REVIEW[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 133-138.
Citation: GONG Ge-lian. LUMINESCENCE DATING FOR ENVIRONMENTAL EVOLUTION STUDY IN TERRESTRIAL LAND,DEEP SEA AND COASTAL BELTS: A REVIEW[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 133-138.

陆地和海洋环境演变研究中的释光测年进展

  • 基金项目:

    中国科学院边缘海地质重点实验室开放基金(MSGLCAS06-2)

详细信息
    作者简介: 龚革联(1967-),男,高级工程师,博士生,从事释光年代学方面的研究工作,E-mail:gg11118@yahoo.com.cn
  • 中图分类号: P597.3

LUMINESCENCE DATING FOR ENVIRONMENTAL EVOLUTION STUDY IN TERRESTRIAL LAND,DEEP SEA AND COASTAL BELTS: A REVIEW

  • 晚全新世以来所发生的特征环境事件的年龄测定,由于研究地区复杂及独特的地质条件,能够充分适用的测年方法有限,而释光测年方法(包括热释光和光释光方法)独有的揭示砂粒级无机成分末次曝光年龄的特点,正好适合于复杂的海岸带沉积环境,并且没有或者较少受到宇宙成因核素年代学分析方法中核素污染等干扰因素的影响。评述了释光测年方法的进展情况,并通过国内外在陆地、海洋和海陆带环境演变响应研究中几个成功运用释光测年方法的案例,分析了这种放射性测年方法的特点,并指出今后释光年代学方法研究的方向。
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出版历程
收稿日期:  2005-10-24
修回日期:  2006-01-09

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