Rutile dating

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This paper reports the results of secondary ion mass spectrometry SIMS U-Pb dating of rutile within eclogitic xenoliths from the Early Cretaceous adakitic rocks in the Xuzhou-Huaibei area of China and discusses the geological significance of these new dates. The former is consistent with the timing of the first stage of exhumation of the Dabie-Sulu orogenic belt and provides evidence of crustal thickening within the southeastern margin of the North China Craton during the early Mesozoic, related to subduction and collision between the Yangtze and North China cratons. The latter age is similar to the timing of emplacement of the hosting intrusion and indicates that the rutile U-Pb system was triggered after uplifting by the intrusion of the hosting magmas. It implies that garnet clinopyroxenite was previously at the depth where the temperature was above the rutile U-Pb closure temperature. This is a preview of subscription content, access via your institution. Rent this article via DeepDyve.
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To browse Academia. Skip to main content. Log In Sign Up. Download Free PDF. Elena Belousova. Download PDF. A short summary of this paper.
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Rutile, often referred throughout history as Red Schorl,is a rare titanium oxide mineral that crystallizes in the form of grains, masses, prismatic crystals and long needle like crystals. These needle shaped crystals can be found penetrating other minerals such as Quartz , Amethyst , and Hematite. These specimens are highly sought after, and often made into jewelry. This crystal is most commonly found as gold or red, but can also be seen as brown or black. Rutile was first discovered in by A.
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Rutile is a common accessory mineral that occurs in a 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. The methods outlined in this paper should find wide application in studies that require age information of single spots, e. This is a preview of subscription content, access via your institution.
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