保加利亚-希腊环罗多坡带东部单元中的变质岩沉积年代综述

N. Bonev, P. Filipov
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引用次数: 0

摘要

Circum-Rhodope带是爱琴海地区北部阿尔卑斯造山带的一个主要构造单元,由变质岩和未变质的与弧有关的侏罗纪埃夫罗斯蛇绿岩组成。在此,我们回顾了保加利亚和希腊环罗多坡带东部不同单元的生物地层学和锆英石年龄。生物地层学和放射性年龄一致显示沉积时间为中三叠世至晚侏罗世。最重要的是,连续的沉积记录勾勒出了来自大陆边缘(罗多佩)和侏罗纪弧系统(埃夫罗蛇绿岩)的沉积物来源,这些沉积物主要由碎屑岩层中的非铁质锆石记录下来。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A review of depositional ages of the metasedimentary rocks in the units of the eastern Circum-Rhodope belt, Bulgaria-Greece
The Circum-Rhodope belt is a major tectonic unit in the Alpine orogen of northern Aegean region, which consists of metasedimentary rocks and unmetamorphosed arc-related Jurassic Evros ophiolite. Here, we review the biostratigraphic and detrital zircon ages available for the distinct units of the eastern Circum-Rhodope belt in Bulgaria and Greece. Both, biostratigraphic and radiometric ages consistently reveal a Middle Triassic to latest Late Jurassic timing of the sedimentation. Most importantly, the continuous depositional record sketches sedimentary sources from the continental margin (Rhodope) and the Jurassic arc system (Evros ophiolite) as documented mostly by the detrital zircons in clastic successions.
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