Zobrazeno 1 - 10
of 29
pro vyhledávání: '"Dušan MAJCIN"'
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 47, Iss 1, Pp 1-22 (2020)
The contribution presents the results of geothermic interpretation approaches applied to measured geothermal data and is focused to determination of the thermal conditions both for application of classic hydrothermal sources exploitation and speciali
Externí odkaz:
https://doaj.org/article/9711cbbf7be34fc8bbec90a5c26b1519
Autor:
Vladimír BEZÁK, Dušan MAJCIN
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 48, Iss 4, Pp 349-363 (2018)
Our contribution presents the geological analysis results of the lithological composition for deep geothermal sources characterized by the thermal conditions suitable for application of classic hydrothermal sources exploitation and specialized EGS te
Externí odkaz:
https://doaj.org/article/c6f7eeafdbbc4c6fa30b3dca6ee861da
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 46, Iss 1, Pp 33-49 (2016)
The contribution presents the results acquired both by direct cognitive geothermic methods and by modelling approaches of the lithosphere thermal state in the region of the Transcarpathian depression and surrounding units. The activities were aimed a
Externí odkaz:
https://doaj.org/article/6a70ced1a1ec462897b215b5c5114cf9
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 45, Iss 3, Pp 193-218 (2015)
The area of the Danube Basin is interesting in the light of the evaluation both of the lithosphere structure and of various theories of Carpathian-Pannonian region tectonic evolution. The aim of this paper is to analyse both the thermal conditions in
Externí odkaz:
https://doaj.org/article/4a322d77bbc14dc0a6fbf6ad88dfeaf4
Autor:
Vladimír BEZÁK, Josef PEK, Dušan MAJCIN, Jana BUČOVÁ, Tomáš ŠOLTIS, Dušan BILČÍK, Radek KLANICA
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 45, Iss 1, Pp 1-11 (2015)
In this paper we present a geological interpretation of magnetotelluric sounding along the southern part of the seismic 2T profile situated in the southern Central Slovakia. The complexes with higher conductivity are imaged in the shallow depths, for
Externí odkaz:
https://doaj.org/article/8d0738ec0e3947478e1df44d79777ec4
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 44, Iss 4, Pp 271-292 (2014)
The locality of the northeastern most part of Slovakian Flysch belt belongs to interesting areas in terms of the interpretation of geothermal conditions in mutual relation with the lithosphere structure and their tectonic development. The evaluation
Externí odkaz:
https://doaj.org/article/2db055d1ba4e4d9db359980b4d421548
Autor:
Milan HVOŽDARA, Dušan MAJCIN
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 43, Iss 1, Pp 39-58 (2013)
We present mathematical modelling of the stationary geothermal field for the three-layered earth which includes a three-dimensional perturbing body below the first layer (over the halfspace substratum). The unperturbed temperature field corresponds t
Externí odkaz:
https://doaj.org/article/759d037f59ef46c18973c60f086dade1
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 42, Iss 4, Pp 283-294 (2012)
A positive gravity anomaly was observed in the Flysch belt realm. Based on this fact and available geological knowledge we suppose that the source of gravity anomaly might be carbonate rocks lying perhaps in the footwall of Flysch sediments. The carb
Externí odkaz:
https://doaj.org/article/9e1c01b410f14b029e533360bc85173c
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 42, Iss 2, Pp 133-159 (2012)
The paper deals with some problems of the heat flow refractions on the subsurface structures with contrasting thermal conductivities. The qualitative and quantitative analyses of these effects were made on the selected structure configurations. Analy
Externí odkaz:
https://doaj.org/article/7827956ab0db4393be17b50430d3d124
Autor:
Milan HVOŽDARA, Dušan MAJCIN
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 41, Iss 3, Pp 211-233 (2011)
We present mathematical modelling of the stationary geothermal field for the two-layered Earth which includes a three-dimensional perturbing body below the first layer (in the substratum). The body is in the form of 3D prismoid with sloping side face
Externí odkaz:
https://doaj.org/article/19aa54021d354c55a2fbf25ae70769eb