Veliki Jastrebac圆顶的伸展拆除(塞尔维亚)

M. Marovic, Ilija Djokovic, M. Toljić, D. Spahić, J. Milivojević
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引用次数: 21

摘要

本文介绍了Veliki Jastrebac圆顶的基本结构元素,以及其形成的变形事件的年代学和机制。确定了Veliki Jastrebac圆顶由两个大序列组成,在垂直剖面上,它们的位置相反。下部为晚白垩世-白垩纪-古近纪低-中变质岩,被古近纪花岗岩类侵入(可能为Vardar带),并被由塞尔维亚-马其顿地块变质岩组成的大型逆冲构造所覆盖。Veliki Jastrebac的低—中变质杂岩与花岗质是古近系在伸展构造作用下挖掘出的变质核杂岩。Apstrakt。U radu su prikazani osnovni elements gra [e] Velikojastreba - ke dome [i] chronologia] meha- nizmi deformation [j] aja odgovornih [j] o .]Utvr| no je da domu izgra|uju dva krupna navla~no-naborna entiteta koja su, u vertical kalnoj sukcesiji, u inversnom poloaju。Dole lee gorwo- kredne i kredno-古近系nisko do sredwometamorfisane steene u koje je utisnut古近系花岗岩(verovatno Vardarska带),gore je krupna navlaka, kristalin Srpsko-makedonske maase。Nisko do sredwe变质岩kompleks Velikog jastreca,花岗岩,prestavqa变质岩核杂岩,ekshumiran mehanizmima ekstenzione tektype of palegenu。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Extensional unroofing of the Veliki Jastrebac dome (Serbia)
This paper presents the basic structural elements of the dome of Veliki Jastrebac, as well as the chronology and mechanisms of the deformational events responsible for its formation. It was determined that the dome of Veliki Jastrebac consists of two large sequences which are, in the vertical section, in the inverse position. The lower part is made of Late Cretaceous and Cretaceous-Palaeogene low-grade to medium-grade metamorphic rocks, which are intruded by Paleogene granitoid (probably the Vardar Zone), which are covered with a large overthrust consisting metamorphics of the Serbian-Macedonian Mass. The low-grade to medium-grade metamorphosed complex of Veliki Jastrebac, with the granitoid, represents a metamorphic core complex, ex- humed by mechanisms of extensional tectonics in the Paleogene. Apstrakt. U radu su prikazani osnovni elementi gra|e Velikojastreba~ke dome i hronologija i meha- nizmi deformacionih doga|aja odgovornih za weno formirawe. Utvr|eno je da domu izgra|uju dva krupna navla~no-naborna entiteta koja su, u vertikalnoj sukcesiji, u inversnom poloaju. Dole lee gorwo- kredne i kredno-paleogene nisko do sredwometamorfisane stene u koje je utisnut paleogeni granitoid (verovatno Vardarska zona), gore je kao krupna navlaka, kristalin Srpsko-makedonske mase. Nisko do sredwe metamorfisan kompleks Velikog Jastrepca sa granitoidom predstavqa metamorfni core com- plex, ekshumiran mehanizmima ekstenzione tektonike u paleogenu.
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