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Oligocene and Lower Miocene source rocks in the Paratethys:palaeogeographical and stratigraphic controls

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F18%3A00000289" target="_blank" >RIV/00025798:_____/18:00000289 - isvavai.cz</a>

  • Result on the web

    <a href="https://doi.org/10.1144/SP464.1" target="_blank" >https://doi.org/10.1144/SP464.1</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1144/SP464.1" target="_blank" >10.1144/SP464.1</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Oligocene and Lower Miocene source rocks in the Paratethys:palaeogeographical and stratigraphic controls

  • Original language description

    Oligocene and Lower Miocene deposits in the Paratethys are important source rocks, but reveal major stratigraphic and regional differences. As a consequence of the &#64257;rst Paratethys isola-tion, source rocks with very good oil potential accumulated during Early Oligocene time in the Cen-tral Paratethys. Coeval source rocks in the Eastern Paratethys are characterized by a lower source potential. With the exception of the Carpathian Basin and the eastern Kura Basin, the source poten-tial of Upper Oligocene and Lower Miocene units is low. In general, this is also valid for rocks formed during the second (Kozakhurian) isolation of the Eastern Paratethys. However, upwelling along a shelf-break canyon caused deposition of proli&#64257;c diatomaceous source rocks in the western Black Sea.Overall, Oligocene–Lower Miocene sediments in the Carpathian Basin (Menilite Formation) can generate up to 10 t HC m&#8722;2. Its high petroleum potential is a consequence of the interplay of very high productivity of siliceous organisms and excellent preservation in a deep silled basin. In con-trast, the petroleum potential of Oligocene–Lower Miocene (Maikopian) sediments in the Eastern Paratethys is surprisingly low (often <2 t HC m&#8722;2). It is, therefore, questionable whether these sed-iments are the only source rocks in the Eastern Paratethys.

  • Czech name

  • Czech description

Classification

  • Type

    C - Chapter in a specialist book

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2018

  • Confidentiality

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

Data specific for result type

  • Book/collection name

    Petroleum Geology of the Black Sea

  • ISBN

    9781786203588

  • Number of pages of the result

    40

  • Pages from-to

    267-306

  • Number of pages of the book

    484

  • Publisher name

    The Geological Society of London

  • Place of publication

    Oxford

  • UT code for WoS chapter