All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Source rock potential of the Miocene sedimentary rocks in the Carpathian Foredeep of the Czech Republic

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F22%3A00000116" target="_blank" >RIV/00025798:_____/22:00000116 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216224:14310/22:00125714

  • Result on the web

    <a href="https://gq.pgi.gov.pl/article/view/32958/pdf" target="_blank" >https://gq.pgi.gov.pl/article/view/32958/pdf</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.7306/gq.1634" target="_blank" >10.7306/gq.1634</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Source rock potential of the Miocene sedimentary rocks in the Carpathian Foredeep of the Czech Republic

  • Original language description

    We determine the organic matter content, its thermal maturity, genetic type, and source rock potential of the Miocene sedimentary rocks in the Czech Carpathian Foredeep. In the Czech Republic the Carpathian Foredeep represents a peripheral foreland basin formed due to the tectonic emplacement and loading of the Alpine-Carpathian Thrust Wedge onto the passive margin of the Bohemian Massif. Random vitrinite/huminite reflectance measurements and maceral analyses were performed on 25 samples from the Carpathian Foredeep succession. Additionally, results of 135 TOC content measurements, 141 Rock-Eval pyrolysis analyses and 27 vitrinite reflectance measurements were used to evaluate the regional distribution and depth trends for the entire Carpathian Foredeep. The thermal maturity of organic matter is between the immature part and peak of the oil window (Tmax = 413–448°C). Beneath the Western Carpathian Thrust Belt, the thermal maturity reaches higher values (Rr = 0.43–0.58percent, Tmax = 429–448°C). The hydrocarbon generation potential is poor or fair, even if the total organic carbon values indicate good or even very good source rock potential. This is mainly due to the prevailing gas-prone Type III kerogen. The best source rocks were observed in the Miocene strata of the southern and central segments of the area discussed.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2022

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Geological Quarterly

  • ISSN

    1641-7291

  • e-ISSN

  • Volume of the periodical

    66

  • Issue of the periodical within the volume

    1 : 1

  • Country of publishing house

    PL - POLAND

  • Number of pages

    16

  • Pages from-to

    nestránkováno

  • UT code for WoS article

    000792119500001

  • EID of the result in the Scopus database

    2-s2.0-85135908436