保加利亚中部罗多坡阿塞尼察和阿尔达单元变质岩中金红石的地球化学--初步结果

Milena Georgieva, Tzvetomila Vladinova
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引用次数: 0

摘要

我们提供了关于保加利亚罗多彼山脉中部阿塞尼察和阿尔达单元变质岩中金红石地球化学的新数据。所研究的金红石中的痕量元素显示出很大的差异,这种差异取决于原岩类型(玄武岩和变质岩)、变质等级、岩石地球化学和矿物关联。金红石中的锌测温法将两个单元的金红石区分开来,阿尔达单元的金红石温度较高(650-750 °C),阿森尼察单元的金红石温度较低(520-630 °C)。大多数金红石的铀含量太低(<0.5 ppm),无法进行铀-铅年代测定。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geochemistry of rutiles from metamorphic rocks of Asenitsa and Arda Units, Central Rhodope, Bulgaria – preliminary results
We present new data on the geochemistry of rutiles from metamorphic rock of the Asenitsa and Arda Units, Central Rhodope Massif, Bulgaria. Trace elements in studied rutiles show large variations that depend on protolith type (metapelites and metabasites), metamorphic grade, the rock geochemistry and mineral association. Zr-in-rutile thermometry distinguishes the rutiles from both units with higher temperatures (650–750 °C) for the Arda Unit and lower temperatures (520–630 °C) for the Asenitsa Unit. The uranium content of most rutiles is too low (<0.5 ppm) for U-Pb dating.
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