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

新手

Quaternary Evolution,In Hungary, according to international practice, we assign the predominantly terrestrial sedimentary formations developed during the last 2.4 Ma of geohistory to the Quaternary.

菊花

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.

对待

Geology and History of Evolution of the Tisza Mega-Unit,the 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

TIA742

大约冬季

Book 2013can 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 geo

intrude

Erika Piazzoli,Rachael Jacobs,Garret Scallynian), Serbian (North Vojvodina) and Romanian (West Transylvanian) territories (Szederkényi 1974, 1984; Kovács 1982; Fülöp 1994; Kovács et al. 2000). In Romania and Croatia large mountains and uplands (Apuseni Mts., Papuk Mts., Psunj Mts.) provide an excellent opportunity to study its structural setting and stratigraphy.

FAR

Geology and History of Evolution of the Tisza Mega-Unit,nian), Serbian (North Vojvodina) and Romanian (West Transylvanian) territories (Szederkényi 1974, 1984; Kovács 1982; Fülöp 1994; Kovács et al. 2000). In Romania and Croatia large mountains and uplands (Apuseni Mts., Papuk Mts., Psunj Mts.) provide an excellent opportunity to study its structural setting and stratigraphy.

背信

Genesis and Evolution of the Pannonian Basin,he Transdanubian region, deposited between the Sarmatian and Pleistocene, and being distinct from both of them. Anyhow, the basin-fill of the Pannonian Basin cannot be confined only to the deposits of Pannonian age; it comprises practically the whole Neogene–Quaternary rock sequence of the area.

北极人

轻信

https://doi.org/10.1007/978-1-349-07082-4he Transdanubian region, deposited between the Sarmatian and Pleistocene, and being distinct from both of them. Anyhow, the basin-fill of the Pannonian Basin cannot be confined only to the deposits of Pannonian age; it comprises practically the whole Neogene–Quaternary rock sequence of the area.