dating rutile

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Rutilethe most abundant of three naturally occurring forms of titanium dioxide TiO 2 ; see also anatase ; brookite. It forms red to reddish brown, hard, brilliant metallic, slender crystals, often dating rutile surrounded by other minerals. Rutile is a commercially important dating rutile mineral, although most titanium dioxide is produced from ilmenite. Rutile has minor uses in porcelain and glass manufacture as a colouring agent and in making some steels and copper alloys.

Thanks for helping us catch any problems with articles on DeepDyve. We'll do our best to fix them. Check all that apply - Please note that only the first page is available if you have not selected a reading option after clicking "Read Article". Include any more information that will help us locate the issue and fix it faster for you. The oldest rocks exposed in this region are variably metamorphosed siliciclastic sedimentary rocks that were deposited in the late Palaeoproterozoic dating rutile intruded episodically by voluminous granitoids and reworked by both local and regional phases of deformation and metamorphism between ca. Collins and Williams, ; Rubatto et al.
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Spot dating of detrital zircon is now routinely dating rutile for provenance work and recently pitfalls of this approach have been published. Zircon, because of its robustness, tends to preserve the age of the igneous event from which it crystallized, and not ensuing metamorphisms that it might have experienced. An advantage of rutile dating is its distain of Th. Essentially if Pb is detected, it is common, and with a model composition, common Pb can be accurately corrected for even if measurement of Pb is not possible. In addition concentrations of Ti and 11 trace elements are measured during dating analysis. Some trace elements Cr, V, and Zr show strong correlation with age.

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This service is more advanced with JavaScript available, learn more at http: Contributions to Mineralogy and Petrology. Rutile is a common accessory mineral that occurs in dating rutile wide spectrum of metamorphic rocks, such as in blueschists, eclogites, and granulites and as one of the most stable detrital heavy minerals in sedimentary rocks. The advent of rutile trace element thermometry has generated increased interest in a better understanding of rutile formation. Rutile thermometry of the same detrital grains indicates former granulite-facies conditions.
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