沿澳大利亚东部从西向东的样带和弗林德斯山脉的一些基岩取样的尘埃U-Th同位素数据

S. Turner , A. Dosseto , P.O. Suresh , M. Turner , H. Handley , P. Hesse
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引用次数: 0

摘要

在本文中,我们介绍了澳大利亚东部沿西向东样带采样的地表尘埃的铀钍(U-Th)同位素数据,以及在样带西端附近的弗林德斯山脉选择的一些基岩样本。尘埃在过去的350年中损失了238U和234U,这意味着化学风化(大量U损失)和物理风化(234U的反冲损失)的结合。近地表基岩并不总是像风化、侵蚀和土壤生产研究中通常假设的那样处于U-Th同位素长期平衡状态。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
U-Th isotope data for dust sampled along a west to east transect in eastern Australia and some bedrock from the Flinders Ranges

In this communication we present Uranium-Thorium (U-Th) isotope data for surficial dusts sampled along a west to east transect in eastern Australia and some selected bedrock samples from the Flinders Ranges near the western end of the transect. The dusts have lost 238U and 234U within the last 350 kyr implying a combination of chemical (bulk U loss) and physical (recoil loss of 234U) weathering. Near-surface bedrock is not always in U-Th isotope secular equilibrium as commonly assumed in studies of weathering, erosion and soil production.

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