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Journal ArticleDOI

Spectroscopic methods applied to zircon

TLDR
A number of spectroscopic techniques have been used to study the properties of natural and synthetic (pure and doped) zircon (ZrSiO4) as mentioned in this paper.
Abstract
Natural and synthetic (pure and doped) zircon (ZrSiO4) have been studied with a variety of spectroscopic techniques. These techniques are based on different physical phenomena, for instance transitions between spin states of nuclei and electrons, energetic transitions of valence electrons, intra-molecular vibrations, or vibrations of atoms and molecular units in the lattice. All of the diverse spectroscopic techniques, however, have in common that they probe energy differences between a ground and excited states, mostly upon interaction of the mineral with incident radiation. Such interactions are not only determined by the excited elementary particles or molecules themselves but depend greatly on their local environments (i.e. number, type, valence and geometrical arrangement of neighboring atoms). Spectroscopic techniques are thus sensitive to the local structure and provide information on the short-range order. Most research on zircon crystals using spectroscopic techniques was done to study their “real structures,” that is the characterization of deviations from “perfect” zircon. Such features include the incorporation of non-formula elements, structural defects and the presence of inclusions and other impurities. Correspondingly, most of the spectroscopic investigations can be assigned to two major groups. The first group represents studies done to characterize the structural position and local environment of non-formula elements when incorporated in the zircon lattice, and accompanying effects on physical properties. The second group comprises studies subjected to the real structures of “metamict” zircon samples, i.e., changes of the zircon structure caused by the impact of self-irradiation and upon recovery from radiation damage (Ewing et al., this volume). It is most obvious that a spectroscopic bulk or point analysis will first of all yield a spectrum (i.e. a plot of the intensity of the respective physical parameter versus wavelength, frequency or wavenumber), and this is what is used in most studies. In addition, image generation based on …

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Enhanced precision, accuracy, efficiency, and spatial resolution of U-Pb ages by laser ablation-multicollector-inductively coupled plasma-mass spectrometry

TL;DR: In this article, the authors studied the transition from Laramide syntectonic sedimentation of the lower Eocene Willwood Formation to post-Laramide volcanogenic sedimentation in the middle Eocene Wapiti Formation in the upper South Fork Shoshone River Valley, Wyoming.
Journal ArticleDOI

Detrital Zircon U-Pb Geochronology Applied to Tectonics

TL;DR: Detrital zircon geochronology is rapidly developing into an essential tool in Earth science research because of the widespread occurrence of detrital minerals in sedimentary systems; the wide range of information that can be extracted from ZIRcon crystals; and the ability to determine ages with reasonable precision, accuracy, and efficiency as discussed by the authors.
Journal ArticleDOI

Zircon: The Metamorphic Mineral

TL;DR: Metamorphic zircon is no longer an impediment to precise geochronology of protolith rocks, but has become a truly indispensable mineral in reconstructing pressure-temperature-time-fluid-paths over a wide range of settings.
Journal ArticleDOI

Laser-ablation split-stream ICP petrochronology

TL;DR: In this paper, a laser-ablation split-stream (LASS) analysis for petrochronology is presented, using dual multi-collector-single collector inductively-coupled plasma mass spectrometry.
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