首页> 外文期刊>Acta Geologica Slovaca >Vek a?litologická charakteristika paleogénnych usadenín Handlovskej kotliny na základe reinterpretácie vrtu FGHn-1 Handlová
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Vek a?litologická charakteristika paleogénnych usadenín Handlovskej kotliny na základe reinterpretácie vrtu FGHn-1 Handlová

机译:基于对FGHn-1Handlová井的重新解释,Handlov盆地古近纪沉积物的年龄和岩性特征

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Handlovská kotlina Basin is filled by Paleogene deposits of the Podtatranská Group. These deposits were previously described as Central Carpathian, Inner Carpathian Paleogene, respectively. The time span of the Paleogene marine sediments was dated from the Middle Eocene (Bartonian) to the Kiscelian. The age of the Huty and Zuberec formations, similarly like in the case of the underlying Terchová Member, was based on the study of microfauna, nannoplankton and large foraminifers. However, recently provided studies on microfauna document, that the upper part of the formation lasts up to the Egerian time. By the revision of microfauna from outcrops in the Huty and Zuberec formations in the Handlovská kotlina Basin we documented a?presence of the Tenuitellinata pseudoedita (Subb.) – a?planctonic species, that's boundary first appearance is from the Egerian time. However, microfaunistic and nannoplancton study (P21–M1 Zones) from FGHn-1 well (10–130?m) can confirms only Paleogene psamites of the Oligocene age.
机译:Handlovskákotlina盆地充满了Podtatranská集团的古近系沉积物。这些矿床先前分别被描述为中喀尔巴阡山脉,内喀尔巴阡山脉古近纪。古近纪海相沉积物的时间跨度是从中始新世(Bartonian)到Kiscelian。 Huty和Zuberec地层的年龄,与下层Terchová成员的情况类似,也是基于微动物群,纳米浮游动物和大型有孔虫的研究而得出的。但是,最近提供的有关微型动物的文献研究表明,地层的上部一直持续到埃格利亚时期。通过对Handlovskákotlina盆地Huty和Zuberec地层露头中的微型动物群的改造,我们记录了Tenuitellinata pseudoedita(Subb。)的存在–一种浮游物种,其边界首次出现是从埃格利亚时代开始的。然而,从FGHn-1井(10-130?m)进行的微功能学和纳米浮游生物研究(P21–M1区)可以确认只有渐新世的古近代角砾岩。

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