Formations of Late Neogene and Pleistocene terrestrial sediments in the region of Mórágy Hill (Hungary)

L. Koloszár, István Marsi
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引用次数: 9

Abstract

In the 1990s detailed geologic exploration in the eastern part of Moragy Hill (Hungary, southeastern Transdanubia) provided a great deal of new knowledge on stratigraphic features. Making use of and reinterpreting all available geologic data, our study gives an overview of the surface and subsurface extent of the Late Neogene and overlying Pleistocene beds, their stratigraphic position, thickness characteristics, as well as lithology, facies and age. We also cover in detail the stratigraphic position, accumulation type and age of the granite rubble, together with the Tengelic Red Clay Formation, previously unknown in the area. A theoretical section of the characteristics of the Paks Loess Formation is shown, based on the data of Moragy Hill and the Tolna Hegyhat Hills, defining and describing its lithological units. Using the large number of accurately evaluated borehole sections in the region it could be proved that the Hungarian loess stratigraphy elaborated by the specialists of the Geographic Research...
匈牙利Mórágy山地区晚新近世和更新世陆相沉积物的形成
20世纪90年代,在Moragy Hill东部(匈牙利外多瑙河东南部)进行了详细的地质勘探,提供了大量关于地层特征的新知识。利用和重新解释所有现有的地质资料,我们对晚新近世和上覆更新世地层的地表和地下范围、地层位置、厚度特征、岩性、相和年龄进行了概述。我们还详细介绍了花岗岩碎石的地层位置、堆积类型和年龄,以及该地区以前未知的腾格里赤粘土组。根据Moragy Hill和Tolna Hegyhat Hills的资料,给出了Paks黄土组特征的理论剖面,定义和描述了其岩性单元。利用该地区大量准确评价的钻孔剖面,可以证明由地理研究中心的专家们详细阐述的匈牙利黄土地层是具有良好地质意义的。
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