Applied Techniques in Marginal and Mature Fields in the Pannonian Basin, Hungary: Case Study

2008 ◽  
Author(s):  
Attila Holoda ◽  
Gyorgy Palasthy
Keyword(s):  
Resources ◽  
2021 ◽  
Vol 10 (4) ◽  
pp. 31
Author(s):  
Stanislav Jacko ◽  
Roman Farkašovský ◽  
Igor Ďuriška ◽  
Barbora Ščerbáková ◽  
Kristína Bátorová

The Pannonian basin is a major geothermal heat system in Central Europe. Its peripheral basin, the East Slovakian basin, is an example of a geothermal structure with a linear, directed heat flow ranging from 90 to 100 mW/m2 from west to east. However, the use of the geothermal source is limited by several critical tectono-geologic factors: (a) Tectonics, and the associated disintegration of the aquifer block by multiple deformations during the pre-Paleogene, mainly Miocene, period. The main discontinuities of NW-SE and N-S direction negatively affect the permeability of the aquifer environment. For utilization, minor NE-SW dilatation open fractures are important, which have been developed by sinistral transtension on N–S faults and accelerated normal movements to the southeast. (b) Hydrogeologically, the geothermal structure is accommodated by three water types, namely, Na-HCO3 with 10.9 g·L−1 mineralization (in the north), the Ca-Mg-HCO3 with 0.5–4.5 g·L−1 mineralization (in the west), and Na-Cl water type containing 26.8–33.4 g·L−1 mineralization (in the southwest). The chemical composition of the water is influenced by the Middle Triassic dolomite aquifer, as well as by infiltration of saline solutions and meteoric waters along with open fractures/faults. (c) Geothermally anomalous heat flow of 123–129 °C with 170 L/s total flow near the Slanské vchy volcanic chain seems to be the perspective for heat production.


2019 ◽  
Author(s):  
M. Vanić ◽  
A. Saprygin ◽  
S. Milojević ◽  
I. Bogatyrev ◽  
A. Polivakho

2017 ◽  
Author(s):  
Artem Polivakho ◽  
Mile Dragosavac ◽  
Kirill Ezhov ◽  
Elena Kharyba ◽  
Ilya Bogatyrev ◽  
...  

2011 ◽  
Vol 26 (2) ◽  
pp. 581-594 ◽  
Author(s):  
Stefan Stauder ◽  
Zoran Stevanovic ◽  
Christian Richter ◽  
Sasa Milanovic ◽  
Andra Tucovic ◽  
...  

Author(s):  
Tomislav Malvić ◽  
Josip Ivšinović ◽  
Josipa Velić ◽  
Rajna Rajić

Presented is semivariogram and the Ordinary Kriging analyses of porosity data from the Sava Depression (Northern Croatia), as part of the Croatian part of the Pannonian Basin System. Data are taken from hydrocarbon reservoirs of the Lower Pontian (Upper Miocene) age, which belongs to the Kloštar-Ivanić Formation. Original datasets had been jack-knifed with purpose to “artificially” increased data and calculate the more reliable semivariograms. The results showed that such improvements can assist in the interpolation of more reliable maps. The both sets, made by original and jack-knifed data, need to be compared using geological recognition of non-allowed shapes (“bull-eyes”, “butterfly effects”) as well as cross-validation results. That comparison made possible to select the most appropriate porosity interpolation.


2017 ◽  
Author(s):  
Artem Polivakho ◽  
Mile Dragosavac ◽  
Kirill Ezhov ◽  
Elena Kharyba ◽  
Ilya Bogatyrev ◽  
...  

2014 ◽  
Vol 11 (11) ◽  
pp. 12271-12290 ◽  
Author(s):  
J. Petrovszki ◽  
G. Timár ◽  
G. Molnár

Abstract. Pre-regulation channel sinuosities of the meandering rivers of the Pannonian Basin are analysed in order to define a mathematical model to estimate the influence of the bankfull discharge and the channel slope on them. As a primary database, data triplets of slope, discharge and sinuosity values were extracted from historical and modern datasets and pre-regulation historical topographic maps. Channel slope values were systematically modified to estimate figures valid before the river regulation works. The bankfull discharges were estimated from the average discharges using a robust yet complex method. The "classical" graphs of Leopold and Wolman (1957), Ackers and Charlton (1970b) and Schumm and Khan (1972) were compiled to a set up a theoretical surface, whose parameters are estimated by the real values of the above database, containing characteristics of the Pannonian Basin rivers. As a result it occurred that there is a two-dimensional function of the bankfull discharges, which provides a good estimation of the most probable sinuosity values of the rivers with the given slope and discharge characteristics. The average RMS error of this estimation is around 15% on this dataset and believed to be the effect of the non-analysed changes in the sediment discharge and size distribution.


2020 ◽  
Author(s):  
A. Gogic ◽  
D. Kundacina ◽  
I. Al-Jeboore

2013 ◽  
Vol XII (1) ◽  
pp. 5-15 ◽  
Author(s):  
Slavoljub Dragićević ◽  
Radislav Tošić ◽  
Milomir Stepić ◽  
Nenad Živković ◽  
Ivan Novković

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