Tectonic setting of the Vardar suture zone (Dinaric-Hellenic belt): the example of the Kopaonik area (southern Serbia)

IF 1.2 4区 地球科学 Q2 GEOLOGY
M. Zélic, M. Marroni, L. Pandolfi, B. Trivic
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引用次数: 16

Abstract

In the tectonic setting of the Dinaric-Hellenic belt, the Vardar Zone is represented by a NW-SE to N-S striking assemblage of oceanic and continental units, each showing different metamorphic grade and deformation features. In this paper, a detailed description of the stratigraphic and structural features of the tectonic units cropping out in the Kopaonik area, belonging to the Vardar Zone of Serbia, is presented. In addition, a 1:50.000 scale geological map of the studied area is also provided. In the Kopaonik area is present a stack of tectonic units, originated during the Alpine deformation phases and referred to both External and Central Vardar Zones of Dimitrijevic´ (1997). These units are represented, from bottom to top, by the Kopaonik Metamorphic Complex, the Brzec´e Unit, the Subophiolite Melange, the Ophiolite Unit and the Brus Unit. The stack of tectonic units is intruded by Early Oligocene granitoids, referred to as the Kopaonik Intrusive Complex. Moreover, the relationships among the tectonic units are unconformably covered by Miocene volcanic rocks and sedimentary deposits. The stratigraphic and structural dataset presented in this paper allows some considerations about the paleogeographic domain of origin for the successions of the different units as well as some interpretations about the tectonic history of the Vardar Zone.
瓦尔达尔缝合带(Dinaric-Hellenic带)的构造背景:以塞尔维亚南部Kopaonik地区为例
在第纳尔—希腊带的构造背景下,瓦尔达尔带以北西—东南—北南走向的洋陆单元组合为代表,各洋陆单元表现出不同的变质程度和变形特征。本文详细描述了塞尔维亚瓦尔达尔带科帕奥尼克地区突出的构造单元的地层和构造特征。此外,还提供了研究区1:50.000比例尺的地质图。在Kopaonik地区存在一叠构造单元,起源于高山变形阶段,涉及Dimitrijevic '(1997)的外部和中央Vardar带。这些单元从下到上依次为:科帕奥尼克变质杂岩、布热克e单元、亚蛇绿岩混杂岩、蛇绿岩单元和布鲁斯单元。该构造单元叠体为早渐新世花岗岩类侵入,称为科帕奥尼克侵入杂岩。此外,构造单元之间的关系被中新世火山岩和沉积物不整合覆盖。本文提供的地层和构造数据可以对不同单元序列的古地理起源域进行一些考虑,并对瓦尔达尔带的构造历史进行一些解释。
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来源期刊
Ofioliti
Ofioliti 地学-地质学
CiteScore
2.40
自引率
7.70%
发文量
1
期刊介绍: Since 1976, Ofioliti provides an international forum for original contributions and reviews in the field of the geodynamics, petrology, geochemistry, biostratigraphy, stratigraphy, tectonics and paleogeography applied to ophiolitic terrains and modern oceanic lithosphere, including their sedimentary cover. Studies of topics such as geodynamics of the mantle, the evolution of orogens including ophiolites and paleoceanography are also welcome
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