发光测年的最新进展及其在日本沉积物中的潜在应用前景

S. Tsukamoto
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引用次数: 1

摘要

综述了近十年来发光测年方法的发展,特别是长石测年技术和岩石表面及埋藏测年的研究进展。长石的红外后IRSL (pRIR)和脉冲IRSL方法已被开发用于减少异常衰落(信号的非热损耗)。在较高的刺激温度下,pRIR信号通常更稳定(衰减较小);然而,信号很难漂白,这对水中沉积物来说是个问题。脉冲IRSL信号具有热稳定性和可快速漂白的优点。还介绍了测量岩石表面和砾石表面暴露和埋藏年龄的新方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Recent developments in luminescence dating and potential future applications to Japanese sediments
The developments in luminescence dating methods, especially regarding feldspar dating techniques and rock surface and burial dating, over the past decade are summarized. Post-IR IRSL (pRIR) and pulsed IRSL methods for feldspar have been developed to reduce anomalous fading (athermal loss of signals). The pRIR signal at higher stimulation temperatures is generally more stable (fades less) ; however, the signal is difficult to bleach, which is problematic for water-lain sediments. The pulsed IRSL signal has both advantages, being athermally stable and quickly bleachable. Newly developed methods for measur-ing surface exposure and burial ages for rock surfaces and gravels are also introduced.
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