Detailed Information on Publication Record

KANALÁŠOVÁ, Soňa, Marek GOLDBACH and Eva GERŠLOVÁ. Subsidence and thermal history of the Uhťice -18 borehole. In CETEG 2015 - 13th Meeting of the Central European Tectonic Groups, Kadaň, Czech Republic. 2015. ISBN 978-80-7075-880-9.

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Basic information
Original name	Subsidence and thermal history of the Uhťice -18 borehole
Authors	KANALÁŠOVÁ, Soňa (203 Czech Republic, belonging to the institution), Marek GOLDBACH (203 Czech Republic, guarantor, belonging to the institution) and Eva GERŠLOVÁ (203 Czech Republic, belonging to the institution).
Edition	CETEG 2015 - 13th Meeting of the Central European Tectonic Groups, Kadaň, Czech Republic, 2015.

Other information
Original language	English
Type of outcome	Conference abstract
Field of Study	10500 1.5. Earth and related environmental sciences
Country of publisher	Czech Republic
Confidentiality degree	is not subject to a state or trade secret
WWW	URL
RIV identification code	RIV/00216224:14310/15:00082752
Organization unit	Faculty of Science
ISBN	978-80-7075-880-9
ISSN	0072-100X
Keywords in English	Subsidence and thermal history; 1D modelling; Uhrice-18 borehole
Changed by	Changed by: Mgr. Marek Goldbach, Ph.D., učo 175459. Changed: 7/5/2015 22:43.

Abstract
The aim of this study was to make a subsidence and thermal history model of the Uhrice 1á borehole, which is situated in the area of the DAmborice highlands in the Outer Western Carpathians. The model was created base on the regional geological concep using Petromod 1D software. As the calibration points Tmax from Rock Eval and trend for vitrinite reflectance were used. The reliability of the model was verified by comparing measured values with simulated.

Abstract

The aim of this study was to make a subsidence and thermal history model of the Uhrice 1á borehole, which is situated in the area of the DAmborice highlands in the Outer Western Carpathians. The model was created base on the regional geological concep using Petromod 1D software. As the calibration points Tmax from Rock Eval and trend for vitrinite reflectance were used. The reliability of the model was verified by comparing measured values with simulated.