Thermal maturity of Miocene organic matter from the Carpathian
Foredeep in the Czech Republic

a 2018

Thermal maturity of Miocene organic matter from the Carpathian Foredeep in the Czech Republic

MEDVECKÁ, Lujza, Eva GERŠLOVÁ, Slavomír NEHYBA a Magdalena MISZ-KENNAN

Základní údaje

Originální název

Thermal maturity of Miocene organic matter from the Carpathian Foredeep in the Czech Republic

Autoři

MEDVECKÁ, Lujza (703 Slovensko, garant, domácí), Eva GERŠLOVÁ (203 Česká republika, domácí), Slavomír NEHYBA (203 Česká republika, domácí) a Magdalena MISZ-KENNAN (616 Polsko)

Vydání

Geologica Balcanica: XXI International Congress of the Carpathian Balkan Geological Association (CBGA), Abstracts, Advances of Geology in southeast European mountain belts, September 10-13, 2018

Další údaje

Jazyk

angličtina

Typ výsledku

Konferenční abstrakt

Obor

10505 Geology

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Kód RIV

RIV/00216224:14310/18:00108982

Organizační jednotka

Přírodovědecká fakulta

ISBN

978-954-90223-8-4

Klíčová slova anglicky

thermal maturity; organic matter; Carpathian Foredeep

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 10. 10. 2019 22:53, Mgr. Lujza Medvecká

Anotace

V originále

The aim of the research was to determine the thermal maturity of the Miocene sedimentary rocks with the vitrinite reflectance. Based on this information, it is possible to characterize the expected paleo-geothermal gradient within the Carpathian Foredeep in the area of Czech Republic. The Carpathian Foredeep represents a peripheral foreland basin formed due to the tectonic emplacement and crustal loading of the Alpine-Carpathian Thrust Wedge onto the passive margin of the Bohemian Massif. The lithological and stratigraphical content and basin architecture changes in different parts of the basin. Local and regional unconformities are developed due to varying intensity and orientation of flexural loading and different geologic and tectonic histories of the basement, along with a polyphase nature of the active basin margin and gradual change of its position. The basin continues north into the Polish part of the Carpathian Foredeep Basin and south into the North Alpine Foreland Basin. 25 samples from 13 boreholes from the central part of the Carpathian Foredeep were collected. For all those samples, random vitrinite reflectance (Rr) was measured and maceral analysis was performed. Additionally, in order to evaluate regional distribution and depth trends for all of the Carpathian Foredeep, an archive data of vitrinite reflectance from 31 samples from 20 boreholes and results of RockEval pyrolysis (RE) from 107 samples were used. The vitrinite reflectance values (% Rr) in boreholes Got 1, Got 2, Tl 1 and Luk 1 are continuously increasing with the depth from 0.36 % Rr to 0.58 % Rr. In samples from Koryčany 9 and 13 boreholes, the vitrinite reflectance ranges from 0.26 % Rr to 0.28 % Rr, and from Mouchnice 1, 2 boreholes, vitrinite reflectance ranges from 0.27 % Rr to 0.29 % Rr. The vitrinite reflectance of organic matter from the boreholes of Ždánice 135, 147, and 175, Snovídky 1 and Žarošice 2 shows significantly lower values (0.22 % Rr – 0.3 % Rr) compared to other parts of the Carpathian Foredeep. Samples also contain a high ratio of organic matter in which liptinite is significantly represented. Maceral analysis of dispersed organic matter in the sediments of the Carpathian Foredeep enabled to determine dominant maceral composition. The analysis showed that the decisive parameter is the ratio of the liptinite component.

Citovat

MEDVECKÁ, Lujza, Eva GERŠLOVÁ, Slavomír NEHYBA a Magdalena MISZ-KENNAN. Thermal maturity of Miocene organic matter from the Carpathian Foredeep in the Czech Republic. In Geologica Balcanica: XXI International Congress of the Carpathian Balkan Geological Association (CBGA), Abstracts, Advances of Geology in southeast European mountain belts, September 10-13. 2018. ISBN 978-954-90223-8-4.

@proceedings{1483862,
   author = {Medvecká, Lujza and Geršlová, Eva and Nehyba, Slavomír and MiszandKennan, Magdalena},
   booktitle = {Geologica Balcanica: XXI International Congress of the Carpathian Balkan Geological Association (CBGA), Abstracts, Advances of Geology in southeast European mountain belts, September 10-13},
   keywords = {thermal maturity; organic matter; Carpathian Foredeep},
   language = {eng},
   isbn = {978-954-90223-8-4},
   title = {Thermal maturity of Miocene organic matter from the Carpathian Foredeep in the Czech Republic},
   year = {2018}
}

TY  - CONF
ID  - 1483862
AU  - Medvecká, Lujza - Geršlová, Eva - Nehyba, Slavomír - Misz-Kennan, Magdalena
PY  - 2018
TI  - Thermal maturity of Miocene organic matter from the Carpathian Foredeep in the Czech Republic
SN  - 9789549022384
KW  - thermal maturity
KW  - organic matter
KW  - Carpathian Foredeep
N2  - The aim of the research was to determine the thermal maturity of the Miocene sedimentary rocks with the vitrinite reflectance. Based on this information, it is possible to characterize the expected paleo-geothermal gradient within the Carpathian Foredeep in the area of Czech Republic. The Carpathian Foredeep represents a peripheral foreland basin formed due to the tectonic emplacement and crustal loading of the Alpine-Carpathian Thrust Wedge onto the passive margin of the Bohemian Massif. The lithological and stratigraphical content and basin architecture changes in different parts of the basin. Local and regional unconformities are developed due to varying intensity and orientation of flexural loading and different geologic and tectonic histories of the basement, along with a polyphase nature of the active basin margin and gradual change of its position. The basin continues north into the Polish part of the Carpathian Foredeep Basin and south into the North Alpine Foreland Basin. 25 samples from 13 boreholes from the central part of the Carpathian Foredeep were collected. For all those samples, random vitrinite reflectance (Rr) was measured and maceral analysis was performed. Additionally, in order to evaluate regional distribution and depth trends for all of the Carpathian Foredeep, an archive data of vitrinite reflectance from 31 samples from 20 boreholes and results of RockEval pyrolysis (RE) from 107 samples were used. The vitrinite reflectance values (% Rr) in boreholes Got 1, Got 2, Tl 1 and Luk 1 are continuously increasing with the depth from 0.36 % Rr to 0.58 % Rr. In samples from Koryčany 9 and 13 boreholes, the vitrinite reflectance ranges from 0.26 % Rr to 0.28 % Rr, and from Mouchnice 1, 2 boreholes, vitrinite reflectance ranges from 0.27 % Rr to 0.29 % Rr. The vitrinite reflectance of organic matter from the boreholes of Ždánice 135, 147, and 175, Snovídky 1 and Žarošice 2 shows significantly lower values (0.22 % Rr – 0.3 % Rr) compared to other parts of the Carpathian Foredeep. Samples also contain a high ratio of organic matter in which liptinite is significantly represented. Maceral analysis of dispersed organic matter in the sediments of the Carpathian Foredeep enabled to determine dominant maceral composition. The analysis showed that the decisive parameter is the ratio of the liptinite component.
ER  -

MEDVECKÁ, Lujza, Eva GERŠLOVÁ, Slavomír NEHYBA a Magdalena MISZ-KENNAN. Thermal maturity of Miocene organic matter from the Carpathian Foredeep in the Czech Republic. In \textit{Geologica Balcanica: XXI International Congress of the Carpathian Balkan Geological Association (CBGA), Abstracts, Advances of Geology in southeast European mountain belts, September 10-13}. 2018. ISBN~978-954-90223-8-4.

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