The lithostratigraphy of the lower Devonian formations of the Eisleck region (northern Luxembourg). Comparison with their Belgian lateral equivalents

IF 1.2 4区 地球科学 Q2 GEOLOGY Geologica Belgica Pub Date : 2017-01-01 DOI:10.20341/gb.2017.001
L. Dejonghe, R. Colbach, E. Goemaere
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引用次数: 3

Abstract

1. IntroductionThe Grand-Duchy of Luxembourg is divided into two main geographical regions, the Eisleck (Oesling in German) to the north (32% of the area) and the Guttland to the south (68% of the area). They correspond to two main geological provinces of the country (Fig. 1).Figure 1. Location map of the studied area.In the Eisleck region, lithostratigraphic units are of lower Devonian (Pragian and Emsian) age; they were folded during the Variscan orogeny) and belong to the SE part of the Ardenne Anticlinorium. From NNW to SSE, the main tectonic structures are: the Houffalize Synclinorium, the Bastogne-Stubach (Stupbach) Anticlinorium, the Neufchâteau-Wiltz-Eifel Synclinorium and the Givonne Anticlinorium. In detail, these large scale structures are complicated by numerous secondary synclines and anticlines.In the Guttland region, lithostratigraphic units belong to the Mesozoic era (Triassic and Jurassic); they are relatively flat-lying and form the northeastern tip of the Paris Basin, the so-called “Gulf of Trier-Luxembourg”.The oldest contribution to geology of the Eisleck region dates back to 1828 and is due to Steininger. The works of Wies (1867) and Wies & Siegen (1877) do not provide a lot of substantial additional information, except on the mineral wealth contained in the grounds of the Eisleck region. The first important contribution concerning the geological subdivisions of the Eisleck region is due to Gosselet (1885). Up to recently, the Luxembourg Devonian stratig
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esisleck地区(卢森堡北部)下泥盆世地层的岩石地层学。与他们的比利时横向等效比较
1. 卢森堡大公国分为两个主要的地理区域,北部的Eisleck(德语为Oesling)占面积的32%,南部的Guttland(占面积的68%)。它们对应于该国的两个主要地质省(图1)。研究区域的位置图。在esisleck地区,岩石地层单元为下泥盆世(Pragian和emian)时代;它们在Variscan造山运动期间被褶皱),属于阿登背斜的东南部分。从NNW到SSE,主要构造为:Houffalize向斜、Bastogne-Stubach (Stupbach)背斜、neufchteau - wiltz - eifel向斜和Givonne背斜。详细地说,这些大型构造被许多次级向斜和背斜复杂化了。在Guttland地区,岩石地层单元属于中生代(三叠纪和侏罗纪);它们相对平坦,形成了巴黎盆地的东北端,即所谓的“特里尔-卢森堡湾”。对埃斯莱克地区地质学最古老的贡献可以追溯到1828年,这要归功于施泰因格。Wies(1867)和Wies & Siegen(1877)的著作并没有提供大量实质性的额外信息,除了关于esisleck地区的矿产资源。关于埃斯莱克地区的地质细分,第一个重要贡献是Gosselet(1885)。直到最近,卢森堡泥盆纪地层
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来源期刊
Geologica Belgica
Geologica Belgica 地学-地质学
CiteScore
4.70
自引率
27.80%
发文量
8
审稿时长
>12 weeks
期刊介绍: Geologica Belgica is a Belgian journal that welcomes papers concerning all aspects of the earth sciences, with a particular emphasis on the regional geology of Belgium, North West Europe and central Africa. Papers not dedicated to the geology of Belgium, North West Europe and central Africa are only accepted when one of the authors is linked to a Belgian University or Institution. Thematic issues are highly appreciated. In this case, guest editors take in charge the selection of the manuscripts and the subject of the papers can be enlarged. The journal is in open access. Submitted manuscripts should be concise, presenting material not previously published. The journal also encourages the publication of papers from Belgian junior authors. Short letters are accepted. Papers written in English are preferred. Each mansucript will be reviewed by at least two reviewers.
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