保加利亚东南部萨卡尔-斯特兰扎带萨卡尔单元最东部三叠纪变质沉积物的地球化学

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
M. Georgieva, Tzvetomila Vladinova
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引用次数: 0

摘要

保加利亚东南部Sakar- strandzha带Sakar单元最东端的三叠纪变质沉积层,其矿物和化学成分从页岩、尾流、岩屑岩到粗砂岩均表现出丰富的多样性。地球化学特征表明其来源风化程度低至中等,上陆壳成分较差。三叠系变质沉积岩为长英质—中火成岩,有一定的再循环沉积输入。在构造背景判别图上,基于不动微量元素,研究的沉积落在大陆岛弧和活动大陆边缘区域。
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 Triassic metasediments from easternmost part of Sakar Unit, Sakar-Strandzha Zone, SE Bulgaria
Triassic metasediments from the easternmost part of Sakar Unit, Sakar-Strandzha Zone, SE Bulgaria, show a high variety in their mineral and chemical composition from shales, wakes, litharenites to arkoses. Geochemical signatures suggest low to moderate weathering degree at their source and upper continental crust composition. The Triassic metasedimentary rocks were derived from felsic to intermediate igneous rocks with some recycled sediment input. On tectonic setting discrimination diagrams, based on immobile trace elements, the studied metasediments fall in the fields of continental island arc and active continental margin.
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