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Titlebook: Geology of Hungary; Janós Haas Book 2013 Springer-Verlag Berlin Heidelberg 2013 Pannonian Basin.geology of Hungary.paleography.regional ge

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发表于 2025-3-21 16:27:39 | 显示全部楼层 |阅读模式
书目名称Geology of Hungary
编辑Janós Haas
视频video
概述Up to date and comprehensive presentation of the geology of Hungary and the Pannonian Basin.Includes many colour images, maps and cross-sections.Invaluable to all geologists.Includes supplementary mat
丛书名称Regional Geology Reviews
图书封面Titlebook: Geology of Hungary;  Janós Haas Book 2013 Springer-Verlag Berlin Heidelberg 2013 Pannonian Basin.geology of Hungary.paleography.regional ge
描述Hungary lies in the central part of the Pannonian Basin, surrounded by the ranges of the Alps, Carpathians, and Dinarides. The geology of the country can be summarized as a process whereby complicated plate collision-type orogeny was followed by the formation of a young basin in which a relatively complete sequence of basin infill has been preserved. The handbook “Geology of Hungary” presents an outline of the main features of the geology and geohistory of the region in a single volume, illustrated by a great number of color figures and photos for the benefit of foreign geoscientists interested in this area. The volume follows the evolutionary history of the major structural units prior to their juxtaposition in the Tertiary and discusses the subsequent evolution of the Pannonian Basin. Due to the geohistorical approach to this study it was necessary to extend the scope of the discussion beyond the present-day political boundaries of Hungary, to cover most of the Pannonian region.
出版日期Book 2013
关键词Pannonian Basin; geology of Hungary; paleography; regional geology; stratigraphy; tectonics
版次1
doihttps://doi.org/10.1007/978-3-642-21910-8
isbn_softcover978-3-662-52088-8
isbn_ebook978-3-642-21910-8Series ISSN 2364-6438 Series E-ISSN 2364-6446
issn_series 2364-6438
copyrightSpringer-Verlag Berlin Heidelberg 2013
The information of publication is updating

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发表于 2025-3-21 23:36:18 | 显示全部楼层
Erika Piazzoli,Rachael Jacobs,Garret Scallythe territory of Hungary the pre-Neogene basement crops out only in two relatively small, isolated areas in South Transdanubia – the Mecsek Mountains and Villány Hills (Figs. 1, 2 in “Introduction”). However, more than three thousand wells, oil and uranium prospecting boreholes provide information o
发表于 2025-3-22 01:30:03 | 显示全部楼层
https://doi.org/10.1007/978-1-349-07082-4n boundaries were coinciding with the Danube. Telegdi-Róth (1879) created the chronostratigraphic concept of the Pannonian age for the formations of the Transdanubian region, deposited between the Sarmatian and Pleistocene, and being distinct from both of them. Anyhow, the basin-fill of the Pannonia
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发表于 2025-3-22 10:23:38 | 显示全部楼层
Geology of Hungary978-3-642-21910-8Series ISSN 2364-6438 Series E-ISSN 2364-6446
发表于 2025-3-22 15:19:09 | 显示全部楼层
Janós HaasUp to date and comprehensive presentation of the geology of Hungary and the Pannonian Basin.Includes many colour images, maps and cross-sections.Invaluable to all geologists.Includes supplementary mat
发表于 2025-3-22 19:19:59 | 显示全部楼层
pathian Units, and the Pelso Composite Unit (northwestern part of the basement of the Pannonian Basin, see Fig. 1.1), which were amalgamated during the Palaeogene to Early Miocene. The name ALCAPA, proposed by Csontos et al. (1992), is derived from the names .ps, .rpathians, and .nnonian Basin.
发表于 2025-3-22 23:40:38 | 显示全部楼层
Geology and History of Evolution of the ALCAPA Mega-Unit,pathian Units, and the Pelso Composite Unit (northwestern part of the basement of the Pannonian Basin, see Fig. 1.1), which were amalgamated during the Palaeogene to Early Miocene. The name ALCAPA, proposed by Csontos et al. (1992), is derived from the names .ps, .rpathians, and .nnonian Basin.
发表于 2025-3-23 05:14:38 | 显示全部楼层
发表于 2025-3-23 09:34:20 | 显示全部楼层
https://doi.org/10.1007/978-3-319-73817-8In Hungary, according to international practice, we assign the predominantly terrestrial sedimentary formations developed during the last 2.4 Ma of geohistory to the Quaternary.
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