2D modelling: A Monte Carlo approach for assessing heterogeneous beta dose rates in luminescence and ESR dating: Paper II, application to igneous rocks

被引:11
作者
Fang, Fang [1 ]
Martin, Loic [2 ]
Williams, Ian S. [1 ]
Brink, Frank [3 ]
Mercier, Norbert [2 ]
Grun, Rainer [1 ,4 ]
机构
[1] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 2601, Australia
[2] Univ Bordeaux Montaigne, Ctr Rech Phys Appl Archeol CRP2A, Inst Rech Archeomat, Maison Archeol,CNRS,UMR 5060, F-33607 Pessac, France
[3] Australian Natl Univ, Ctr Adv Microscopy, Canberra, ACT 2601, Australia
[4] Griffith Univ, Australian Res Ctr Human Evolut, Nathan, Qld 4111, Australia
关键词
Dose rate; Modelling; Thermochronology; Igneous rock; Mineral mapping; QUARTZ; CATHODOLUMINESCENCE; ATTENUATION; ALLANITE; SAMPLES; ZIRCON; GRAINS; REE; TH;
D O I
10.1016/j.quageo.2018.07.005
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Accurate evaluations of beta dose rates are crucial in luminescence and electron spin resonance (ESR) thermochronology. Most igneous rocks are heterogeneous and have complex mineralogical structures that render them unsuitable for the conventional methods of beta dose rate calculations based on infinite matrix assumptions. The recently developed software DosiVox-2D provides a Monte-Carlo approach for calculating beta dose rates in realistic heterogeneous geometries. In this paper, we present 2D simulations of uniform and layered igneous rocks. For the modelling, mineral distribution maps were obtained by QEM-EDS (quantitative evaluation of minerals using energy dispersive spectroscopy) and radionuclide concentrations in minerals were determined by laser ablation (LA) ICP-MS. The results show that the skewness of beta dose rate distributions in quartz reduces as the K concentration in a rock increases, and the estimation of the beta dose rate can be critically influenced by the U and Th concentrations and distributions.
引用
收藏
页码:195 / 206
页数:12
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