Vernaricum -区域分布、岩石地层学、构造和古地理

Q3 Earth and Planetary Sciences

Mineralia Slovaca Pub Date : 2023-07-31 DOI:10.56623/ms.2023.55.1.1

J. Hók, M. Olšavský

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引用次数: 0

摘要

Vernaricum是属于喀尔巴阡山脉西部内部的时间推覆体系统的最高部分单位。Vernaricum沉积物的地层范围为下三叠统至下侏罗统。二叠纪流纹岩和火山碎屑岩在构造上与下三叠统沉积物相结合。Vernaricum位于Veporicum北部、Fatricum、Hronicum下部部分推覆体和Veporicum南部的构造单元上。泛绿岩、美利亚岩和硅质岩杂岩位于构造覆盖层中。Vernaricum的古地理位置在Veporic带和generic带之间。

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Vernaricum ‒ regional distribution, lithostratigraphy, tectonics and paleogeography

The Vernaricum is the highest partial unit belonging to the Hronic nappe system of the Internal Western Carpathians. The stratigraphic range of the Vernaricum sediments is from the Lower Triassic to the Lower Jurassic. The Permian rhyolites and volcaniclastics are tectonically incorporated into the Lower Triassic sediments. The Vernaricum overlies tectonic units of the Northern Veporicum, Fatricum, lower partial nappes of Hronicum and Southern Veporicum. The Gemeric, Meliatic and Silicic rock complexes are located in the tectonic overburden. The paleogeographic position of the Vernaricum is interpreted between the Veporic and Gemeric zones.

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来源期刊

Mineralia Slovaca Earth and Planetary Sciences-Geotechnical Engineering and Engineering Geology

CiteScore

0.60

自引率

0.00%

发文量

期刊介绍： Mineralia Slovaca is a scientific peer-reviewed journal, published by the State Geological Institute of Dionýz Štúr in printed and online versions. The journal publishes original scientific papers, expanding the boundaries of knowledge within the geosciences. It is issued since 1969. Archive of articles on Mineralia Slovaca website enables the online access to full-text papers of all previous years.