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Journal ArticleDOI

Helium diffusion in natural zircon: radiation damage, anisotropy, and the interpretation of zircon (U-TH)/He thermochronology

01 Mar 2013-American Journal of Science (Yale University)-Vol. 313, Iss: 3, pp 145-198
TL;DR: In this article, the authors present a series of date and diffusion measurements that document the importance of alpha dose, which they interpret to be correlated with accumulated radiation damage, on He diffusivity.
Abstract: Accurate thermochronologic interpretation of zircon (U-Th)/He dates requires a realistic and practically useful understanding of He diffusion kinetics in natural zircon, ideally across the range of variation that characterize typically dated specimens. Here we present a series of date and diffusion measurements that document the importance of alpha dose, which we interpret to be correlated with accumulated radiation damage, on He diffusivity. This effect is manifest in both date-effective uranium (eU) correlations among zircon grains from single hand samples and in diffusion experiments on pairs of crystallographically oriented slabs of zircon with alpha doses ranging from ∼1016 to 1019 α/g. We interpret these results as due to two contrasting effects of radiation damage in zircon, both of which have much larger effects on He diffusivity and thermal sensitivity of the zircon (U-Th)/He system than crystallographic anisotropy. Between 1.2 × 1016 α/g and 1.4 × 1018 α/g, the frequency factor, D0, measured in the c-axis parallel direction decreases by roughly four orders of magnitude, causing He diffusivity to decrease dramatically (for example by three orders of magnitude at temperatures between 140 and 220 °C). Above ∼2 × 1018 α/g, however, activation energy decreases by a factor of roughly two, and diffusivity increases by about nine orders of magnitude by 8.2 × 1018 α/g. We interpret these two trends with a model that describes the increasing tortuosity of diffusion pathways with progressive damage accumulation, which in turn causes decreases in He diffusivity at low damage. At high damage, increasing diffusivity results from damage zone interconnection and consequential shrinking of the effective diffusion domain size. Our model predicts that the bulk zircon (U-Th)/He closure temperature (Tc) increases from about 140 to 220 °C between alpha doses of 1016 to 1018 α/g, followed by a dramatic decrease in Tc above this dose. Linking this parameterization to one describing damage annealing as a function of time and temperature, we can model the coevolution of damage, He diffusivity, and (U-Th)/He date of zircon. This model generates positive or negative date-eU correlations depending on the extent of damage in each grain and the date-eU sample9s time-temperature history.
Citations
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Journal ArticleDOI
TL;DR: The basic principles of radiometric geochronology as implemented in a new software package called IsoplotR, which was designed to be free, flexible and future-proof, are reviewed.
Abstract: This paper reviews the basic principles of radiometric geochronology as implemented in a new software package called IsoplotR, which was designed to be free, flexible and future-proof. IsoplotR is free because it is written in non-proprietary languages (R, Javascript and HTML) and is released under the GPL license. The program is flexible because its graphical user interface (GUI) is separated from the command line functionality, and because its code is completely open for inspection and modification. To increase future-proofness, the software is built on free and platform-independent foundations that adhere to international standards, have existed for several decades, and continue to grow in popularity. IsoplotR currently includes functions for U-Pb, Pb-Pb, 40 Ar/ 39 Ar, Rb-Sr, Sm-Nd, Lu-Hf, Re-Os, U-Th-He, fission track and U-series disequilibrium dating. It implements isochron regression in two and three dimensions, visualises multi-aliquot datasets as cumulative age distributions, kernel density estimates and radial plots, and calculates weighted mean ages using a modified Chauvenet outlier detection criterion that accounts for the analytical uncertainties in heteroscedastic datasets. Overdispersion of geochronological data with respect to these analytical uncertainties can be attributed to either a proportional underestimation of the analytical uncertainties, or to an additive geological scatter term. IsoplotR keeps track of error correlations of the isotopic ratio measurements within aliquots of the same samples. It uses a statistical framework that will allow it to handle error correlations between aliquots in the future. Other ongoing developments include the implementation of alternative user interfaces and the integration of IsoplotR with other data reduction software.

1,320 citations


Cites background from "Helium diffusion in natural zircon:..."

  • ..., 2015), radiation damage (Flowers et al., 2009; Guenthner et al., 2013), and breakage during mineral separation (Brown et al....

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Journal ArticleDOI
TL;DR: The role of rift-related processes in subsequent collision is captured by inverse modeling of thermochronological data, using relationship between zircon (U-Th-Sm)/He ages and uranium content, combined with a thermo-kinematic models of a rift-orogen cycle as discussed by the authors.

113 citations

Journal ArticleDOI
TL;DR: In this article, the authors quantify the impact of intrinsic bias on detrital studies thanks to the analysis of modern detritus shed from the European Alps, and illustrate the general implications on geological interpretations.

112 citations

Journal ArticleDOI
TL;DR: In this paper, low-temperature thermochronological data from 80 samples in eastern Kyrgyzstan are combined with previously published data from 61 samples to constrain exhumation in a number of mountain ranges in the Central Kyrgytz Tien Shan.
Abstract: New low-temperature thermochronological data from 80 samples in eastern Kyrgyzstan are combined with previously published data from 61 samples to constrain exhumation in a number of mountain ranges in the Central Kyrgyz Tien Shan. All sampled ranges are found to have a broadly consistent Cenozoic exhumation history, characterized by initially low cooling rates (<1°C/Myr) followed by a series of increases in exhumation that occurred diachronously across the region in the late Cenozoic that are interpreted to record the onset of deformation in different mountain ranges. Combined with geological estimates for the onset of proximal deformation, our data suggest that the Central Kyrgyz Tien Shan started deforming in the late Oligocene-early Miocene, leading to the development of several, widely spaced mountain ranges separated by large intermontane basins. Subsequently, more ranges have been constructed in response to significant shortening increases across the Central Kyrgyz Tien Shan, notably in the late Miocene. The order of range construction is interpreted to reflect variations in the susceptibility of inherited structures to reactivation. Reactivated structures are also shown to have significance along strike variations in fault vergence and displacement, which have influenced the development and growth of individual mountain ranges. Moreover, the timing of deformation allows the former extent of many intermontane basins that have since been partitioned to be inferred; this can be linked to the highly time-transgressive onset of late Cenozoic coarse clastic sedimentation.

108 citations


Cites background from "Helium diffusion in natural zircon:..."

  • ...damage [Reiners et al., 2004; Shuster et al., 2006; Flowers et al., 2007; 2009; Guenthner et al., 2013], or for AHe, the number of intact crystal terminations [Brown et al....

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  • ...147 damage [Reiners et al., 2004; Shuster et al., 2006; Flowers et al., 2007; 2009; Guenthner et al., 2013], or for AHe, the number of intact crystal terminations [Brown et al., 2013] (see supporting information for relevant parameters)....

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Journal ArticleDOI
TL;DR: The technique provides new insights into fluid inclusions as potential traps of radiogenic He and confirms the effect of heterogeneity in parent-daughter isotope abundances and metamictization on (U-Th)/He systematics.
Abstract: Zircon (U-Th)/He thermochronometry is an established radiometric dating technique used to place temporal constraints on a range of thermally sensitive geological events, such as crustal exhumation, volcanism, meteorite impact, and ore genesis. Isotopic, crystallographic, and/or mineralogical heterogeneities within analyzed grains can result in dispersed or anomalous (U-Th)/He ages. Understanding the effect of these grain-scale phenomena on the distribution of He in analyzed minerals should lead to improvements in data interpretation. We combine laser ablation microsampling and noble gas and trace element mass spectrometry to provide the first two-dimensional, grain-scale zircon He “maps” and quantify intragrain He distribution. These maps illustrate the complexity of intracrystalline He distribution in natural zircon and, combined with a correlated quantification of parent nuclide (U and Th) distribution, provide an opportunity to assess a number of crystal chemistry processes that can generate anomalous zircon (U-Th)/He ages. The technique provides new insights into fluid inclusions as potential traps of radiogenic He and confirms the effect of heterogeneity in parent-daughter isotope abundances and metamictization on (U-Th)/He systematics. Finally, we present a new inversion method where the He, U, and Th mapping data can be used to constrain the high- and low-temperature history of a single zircon crystal.

108 citations


Cites background or methods from "Helium diffusion in natural zircon:..."

  • ...Plausible explanations for this included heterogeneous distribution of parent nuclides and fragmentation of crystals (both complicating routine a-ejection correction) (11, 21, 29–33), radiation damage affectingHe retentivity and closure temperature (10, 34), and inclusions containing “excess” He (11, 35, 36)....

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  • ...(10) corresponding to the thermal trajectories from (B) (color-coded)....

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  • ...Intracrystal heterogeneity of radiation damage Intracrystal variation in the degree of radiationdamage can result in both positive and negative correlations between eU concentration and He retention (10, 40)....

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  • ...This example allows a visual comparison between domains of zircon crystal damage and He abundance, reflecting differential He retentivity as a result of the metamictization process (10, 34)....

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  • ...(10) was opted tomodelHe diffusion in zircon....

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References
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Book
25 May 1984
TL;DR: An overview of diffusion and separation processes brings unsurpassed, engaging clarity to this complex topic as mentioned in this paper, which is a key part of the undergraduate chemical engineering curriculum and at the core of understanding chemical purification and reaction engineering.
Abstract: This overview of diffusion and separation processes brings unsurpassed, engaging clarity to this complex topic. Diffusion is a key part of the undergraduate chemical engineering curriculum and at the core of understanding chemical purification and reaction engineering. This spontaneous mixing process is also central to our daily lives, with importance in phenomena as diverse as the dispersal of pollutants to digestion in the small intestine. For students, Diffusion goes from the basics of mass transfer and diffusion itself, with strong support through worked examples and a range of student questions. It also takes the reader right through to the cutting edge of our understanding, and the new examples in this third edition will appeal to professional scientists and engineers. Retaining the trademark enthusiastic style, the broad coverage now extends to biology and medicine.

5,195 citations


"Helium diffusion in natural zircon:..." refers background in this paper

  • ...This is analogous to diffusion in a porous medium where effective diffusivity is expressed as (Cussler, 1984): De Dz ....

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Journal ArticleDOI
TL;DR: In this paper, two low-temperature thermochronometers, namely fission-track and (U-Th)/He, are discussed, and a forward and inverse model solution is proposed.
Abstract: The thermochronometric systems discussed in this volume broadly share three features: parent isotopes, daughter products, and one or more time-dependent, temperature-sensitive processes by which daughter products are altered or lost. If these processes can be measured in the laboratory, and their behavior confidently extrapolated to geological time scales, it becomes possible to construct a forward model of the system that predicts how a given instance of it will evolve assuming a particular starting arrangement and subsequent time-temperature history. Once a forward model has been created and verified, it then becomes possible to apply it in the inverse sense: given a measured ending condition and an assumed starting one, find the intervening time-temperature history. In general, because of information loss, limited precision of measurements, and lack of system uniqueness, more than one history is consistent with a given ending condition. As a result, an inverse model solution usually consists of a set of thermal histories that are consistent with the measured data, as judged by some statistical criterion. This chapter will concentrate on two low-temperature thermochronometers: fission-track (primarily for apatite) and (U-Th)/He. All of the calculations described here are implemented in a computer program called “HeFTy,” which is available with this volume (see Ehlers et al. 2005). A theme that will be touched upon throughout this chapter is that forward and inverse models are only as good as the data and assumptions behind them. Although this principle of course holds for all scientific investigations, it is often obscured when such details are packaged in user-friendly software that produces publication-ready graphics. Fission tracks form continuously over time at a rate dependent solely upon the concentration of uranium present. Earlier-formed fission tracks tend to be shorter than later-formed tracks, as they will have had more time to anneal, and may have experienced …

1,107 citations


"Helium diffusion in natural zircon:..." refers methods in this paper

  • ...For each zoned zircon, we model the uncorrected date, the FTZ corrected date using the “redistribution” option in HeFTy, and the FTH corrected date....

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  • ...However, we discuss below the results from several HeFTy models to show how zonation affects differential damage accumulation within a zircon and sample date-eU correlations....

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  • ...This issue can be dealt with by using a zoned alpha ejection correction (FTZ) that accounts for alpha particle redistribution, which is an option in HeFTy....

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  • ...With an estimate of the diffusion coefficient from equation (8), we then solve the diffusion equation numerically for a spherical geometry with the Crank-Nicholson finite difference scheme used in the thermal modeling software package HeFTy (Ketcham, 2005)....

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Journal ArticleDOI
TL;DR: A mathematical framework for quantitative evaluation of alpha-stopping effects on (U-Th)/He ages has been developed in this paper, and the results are useful for identifying the size and shape of grains which are best suited for (UTh/He) dating and provide the basis for correcting ages when ejection effects are significant.

1,096 citations

Journal ArticleDOI
TL;DR: In this paper, high-precision stepped-heating experiments were performed to better characterize helium diffusion from apatite using Durango fluorapatite as a model system.
Abstract: High-precision stepped-heating experiments were performed to better characterize helium diffusion from apatite using Durango fluorapatite as a model system. At temperatures below 265°C, helium diffusion from this apatite is a simple, thermally activated process that is independent of the cumulative fraction of helium released and also of the heating schedule used. Across a factor of ∼4 in grain size, helium diffusivity scales with the inverse square of grain radius, implying that the physical grain is the diffusion domain. Measurements on crystallographically oriented thick sections indicate that helium diffusivity in Durango apatite is nearly isotropic. The best estimate of the activation energy for He diffusion from this apatite is E_a = 33±0.5 kcal/mol, with log(D_0) = 1.5±0.6 cm^2/s. The implied He closure temperature for a grain of 100 μm radius is 68°C assuming a 10°C/Myr cooling rate; this figure varies by ±5°C for grains ranging from 50 to 150 μm radius. When this apatite is heated to temperatures from 265 to 400°C, a progressive and irreversible change in He diffusion behavior occurs: Both the activation energy and frequency factor are reduced. This transition in behavior coincides closely with progressive annealing of radiation damage in Durango apatite, suggesting that defects and defect annealing play a role in the diffusivity of helium through apatite.

954 citations


"Helium diffusion in natural zircon:..." refers background in this paper

  • ...…or ones similar to it, has been observed previously in zircon (Reiners and others, 2002; Reiners and others, 2004) and several other minerals, including titanite (Reiners and Farley, 1999), goethite (Shuster and others, 2005), magnetite (Blackburn and others, 2007), and apatite (Farley, 2000)....

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  • ...These traps sequester He (governed by an equilibrium partition coefficient) and prevent or slow its diffusive migration out of the crystal (Farley, 2000)....

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Journal ArticleDOI
TL;DR: Shuster et al. as discussed by the authors developed and investigated a new kinetic model, the radiation damage accumulation and annealing model (RDAAM), that adopts the effective fission track density as a proxy for accumulated radiation damage.

755 citations