Results 101 to 110 of about 1,330 (202)
Bryoherms from the lower Sarmatian (upper Serravallian, Middle Miocene) of the Central Paratethys. [PDF]
Piller WE, Harzhauser M.
europepmc +1 more source
Badenian discoasters from the section in Lenart (Northeast Slovenia, Central Paratethys)
In Slovenske gorice, south of Lenart, a 20 m profile of Middle Miocene strata has been exposed. During previous research numerous discoasters have been found among other coccoliths. In Slovenia Miocene discoasters have only been found in Badenian sedimentsin Slovenske gorice and they are particularly useful for paleoecological reconstructions ...
Miloš Bartol, Jernej Pavšič
openaire +2 more sources
Spatial development of the Badenian sediments thickness reflects tectono-erosional stage of the pre-Badenian relief in combination with advancing orogenic front of the Outer Western Carpathians.
Wlosok, Jiří +2 more
core
Exploring the Effects of Residence Time on the Utility of Stable Isotopes and S/C Ratios as Proxies for Ocean Connectivity. [PDF]
Stüeken EE, Viehmann S, Hohl SV.
europepmc +1 more source
Geological structure and hydrogeologic conditions of the Herlany geyser structure (Eastern Slovakia) [PDF]
Analysis of new geological data from the surroundings of Herlany resulted in a new concept of geological structure and partly also of Herlany geyser`s mechanism. The concept in based on freatic water percolation and saturation by carbon dioxide ascending
Magyar Július, Rudinec Rudolf
doaj
Multi-Level Sensing Technologies in Landslide Research-Hrvatska Kostajnica Case Study, Croatia. [PDF]
Podolszki L +3 more
europepmc +1 more source
Calculating dissolved marine oxygen values based on an enhanced Benthic Foraminifera Oxygen Index. [PDF]
Kranner M +4 more
europepmc +1 more source
Origin of the Badenian salts from East Slovakian basin indicated by the analysis of fluid inclusions
Chemical composition of the brines of primary fluid inclusions in sedimentary halite (from the boreholes: P-2, P-3, P-6, P-7 and P-8) of the Badenian evaporite of the Zbudza Fm. from East Slovakian basin indicates that the basinal brines belong to the Na-
Bukowski, K. +4 more
core
The Pogórska Wola palaeovalley of combined tectonic and erosional origin dissects the Mesozoic floor of the Carpathian Foredeep Basin to a depth exceeding 1200 m.
Głuszyński, A., Aleksandrowski, P.
core +1 more source
На основі досліджень палео- та сучасних гідрогеологічних умов верхньобаденського горизонту Зовнішньої зони Передкарпатського прогину розкрито основні закономірності формування і збереження його газових покладів.
Лук’янчук, Д. +1 more
core

