The inclusion of grothite in the zircon from granitoids of the crystalline basement of the Southern Yamal peninsula

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Grothite - rare F-Al-rich type of titanite - has been found in accessory zircon from the granitoids of the pre-Jurassic basement of the Verkhnerechensky oil-gas area (in the southern part of the Yamal Peninsula) as a result of the study. Titanite forms rare inclusions (so-called minerals-prisoners) in the central parts of zircon crystals; in our sample of 35 individuals only two grains of titanite have been discovered. The measurement of the chemical composition of the mineral has been carried out on an electron-probe microanalyzer CAMECA SX 100, equipped with five wave spectrometers (IGG UrB RAS, Ekaterinburg). According to the microprobe analysis, the mineral has an unusual chemical composition, it shows the presence of significant concentrations of alumina (Al2O3 to 8.5 wt.%), rare earths elements (REE to 4.3 wt.%), and fluorine (F to 2 wt.%). This grothite is dramatically different in chemical composition from the accessory titanite of the matrix granitoid (monzoleicogranite), which is characterized by values close to the reference sphene...

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Grothite, zircon, granitoid, pre-jurassic foundation, south yamal, arctic

Короткий адрес: https://sciup.org/142220006

IDR: 142220006   |   DOI: 10.21443/1560-9278-2019-22-1-5-11

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