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Zircon is a part of the ZTR index to classify highly- weathered sediments. Zircon is a common accessory to trace mineral constituent of most granite and felsic igneous rocks. Due to its hardness, durability and chemical inertness, zircon persists in sedimentary deposits and is a common constituent of most sands. Zircon is rare within mafic rocks and very rare within ultramafic rocks aside from a group of ultrapotassic intrusive rocks such as kimberlites , carbonatites, and lamprophyre, where zircon can occasionally be found as a trace mineral owing to the unusual magma genesis of these rocks.
Zircon forms economic concentrations within heavy mineral sands ore deposits , within certain pegmatites , and within some rare alkaline volcanic rocks, for example the Toongi Trachyte, Dubbo, New South Wales Australia  in association with the zirconium-hafnium minerals eudialyte and armstrongite. Zircon has played an important role during the evolution of radiometric dating.
Zircon Dating - ScienceAid
Because zircons can survive geologic processes like erosion , transport, even high-grade metamorphism , they contain a rich and varied record of geological processes. For instance, imaging the cathodoluminescence emission from fast electrons can be used as a prescreening tool for high-resolution secondary-ion-mass spectrometry SIMS to image the zonation pattern and identify regions of interest for isotope analysis. This is done using an integrated cathodoluminescence and scanning electron microscope. In addition, the oxygen isotopic compositions of some of these zircons have been interpreted to indicate that more than 4.
SEM image of zircon. From Wikipedia, the free encyclopedia. Zirconium silicate, a mineral belonging to the group of nesosilicates. Not to be confused with zirconia , cubic zirconia , or zirconium.
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This article is about the mineral. For other uses, see Zircon disambiguation. A lustrous crystal of zircon perched on a tan matrix of calcite from the Gilgit District of Pakistan. Handbook of Mineralogy PDF. Mineralogical Society of America. Retrieved April 29, A Guide to the Elements.
Retrieved 7 October Retrieved April 29, — via www. Evidence for extensive weathering of Earth's earliest crust". Earth and Planetary Science Letters.
Archived from the original on 23 October Retrieved 8 October National Academy of Sciences. Early edition, published online before print.
Reviews in Mineralogy and Geochemistry , Neues Jahrbuch Mineralogische Monatshefte. This effect is referred to as discordance and is demonstrated in Figure 1. If a series of zircon samples has lost different amounts of lead, the samples generate a discordant line. The upper intercept of the concordia and the discordia line will reflect the original age of formation, while the lower intercept will reflect the age of the event that led to open system behavior and therefore the lead loss; although there has been some disagreement regarding the meaning of the lower intercept ages.
Zircon is very chemically inert and resistant to mechanical weathering—a mixed blessing for geochronologists, as zones or even whole crystals can survive melting of their parent rock with their original uranium-lead age intact. Zircon crystals with prolonged and complex histories can thus contain zones of dramatically different ages usually, with the oldest and youngest zones forming the core and rim, respectively, of the crystal , and thus are said to demonstrate inherited characteristics.
Unraveling such complications which, depending on their maximum lead-retention temperature, can also exist within other minerals generally requires in situ micro-beam analysis via, say, ion microprobe SIMS or laser ICP-MS.
From Wikipedia, the free encyclopedia. The disintegration products of uranium: American Journal of Science Retrieved 7 January Alpha-recoil in U-Pb geochronology: Effective sample size matters.
Contributions to Mineralogy and Petrology , 4: Combined annealing and multi-step dissolution analysis for Improved precision and accuracy of zircon ages. Radiogenic Isotope Geology 2nd ed.
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Deep time Geological history of Earth Geological time units. Chronostratigraphy Geochronology Isotope geochemistry Law of superposition Luminescence dating Samarium—neodymium dating. Amino acid racemisation Archaeomagnetic dating Dendrochronology Ice core Incremental dating Lichenometry Paleomagnetism Radiometric dating Radiocarbon Uranium—lead Potassium—argon Tephrochronology Luminescence dating Thermoluminescence dating.
Fluorine absorption Nitrogen dating Obsidian hydration Seriation Stratigraphy. Retrieved from " https: Wikipedia articles needing clarification from October Views Read Edit View history.
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