Petroleum Geology of the Black Sea
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The Black Sea remains one of the largest underexplored rift basins in the world. Future success is dependent on a better understanding of a number of geological uncertainties. These include reservoir and source rock presence and quality, and the timing of migration of hydrocarbons relative to trap formation. An appreciation of the geological history of the Black Sea basins and the surrounding orogens is therefore key. The timing of basin formation, uplift of the margins, and of facies distribution remain issues for robust debate. This Special Publication presents the results of 15 studies that relate to the tectono-stratigraphy and petroleum geology of the Black Sea. The methodologies of these studies encompass crustal structure, geodynamic evolution, stratigraphy and its regional correlation, petroleum systems, source to sink, hydrocarbon habitat and play concepts, and reviews of past exploration. They provide insight into the many ongoing controversies concerning Black Sea regional geology and provide a better understanding of the geological risks that must be considered for future hydrocarbon exploration.
Source potential and depositional environment of Oligocene and Miocene rocks offshore Bulgaria
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Published:January 01, 2018
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CiteCitation
J. Mayer, B. J. Rupprecht, R. F. Sachsenhofer, G. Tari, A. Bechtel, S. Coric, W. Siedl, W. Kosi, J. Floodpage, 2018. "Source potential and depositional environment of Oligocene and Miocene rocks offshore Bulgaria", Petroleum Geology of the Black Sea, M. D. Simmons, G. C. Tari, A. I. Okay
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Abstract
Oligo-Miocene (‘Maikopian’) deposits are considered the main source rocks in the Black Sea area, although only a few source-rock data are available. Geochemical logs from nine wells are used together with age constraints provided by calcareous nannoplankton, well and seismic data to determine vertical and lateral changes of the source potential. Oligocene rocks overlie Eocene deposits with a major unconformity on the western Black Sea shelf in Bulgaria. A west–east-trending erosional structure (the Kaliakra canyon) developed during Lower Oligocene time and was filled with Oligo-Miocene deposits. Potential source rocks are present in different stratigraphic units, but the most prolific...
- algae
- aliphatic hydrocarbons
- alkanes
- biomarkers
- Black Sea region
- brackish-water environment
- Bulgaria
- Cenozoic
- chemical composition
- chromatograms
- depositional environment
- diatoms
- erosional unconformities
- Europe
- framework silicates
- gas chromatograms
- geophysical methods
- geophysical profiles
- geophysical surveys
- hydrocarbons
- hydrogen
- isolation
- macerals
- Maikop Series
- microfossils
- microscope methods
- Miocene
- nannofossils
- nannoplankton
- Neogene
- offshore
- Oligocene
- opal
- opal-A
- organic compounds
- Paleogene
- paleosalinity
- Paratethys
- petroleum
- phytane
- plankton
- Plantae
- potential deposits
- pristane
- productive capacity
- productivity
- pyrolysis
- sea-level changes
- sedimentary rocks
- sediments
- seismic methods
- seismic profiles
- silica minerals
- silicates
- source rocks
- Southern Europe
- stratigraphic units
- surveys
- Tertiary
- thermal maturity
- total organic carbon
- unconformities
- well logs
- Kaliakra Canyon