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.
Geochronology, geochemistry and isotope systematics of a mafic–intermediate dyke complex in the İstanbul Zone. New constraints on the evolution of the Black Sea in NW Turkey
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Published:January 01, 2018
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CiteCitation
Namık Aysal, Mehmet Keskin, Irena Peytcheva, Olgun Duru, 2018. "Geochronology, geochemistry and isotope systematics of a mafic–intermediate dyke complex in the İstanbul Zone. New constraints on the evolution of the Black Sea in NW Turkey", Petroleum Geology of the Black Sea, M. D. Simmons, G. C. Tari, A. I. Okay
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Abstract
We report new U–Pb zircon ages, major and trace element data, mineral chemistry, and Sr–Nd isotopic analyses of the mafic–intermediate dykes and intrusions in the İstanbul Zone. Mafic dykes are represented by calc-alkaline to alkaline lamprophyre and diabase. Intermediate dykes and subvolcanics are andesitic to dacitic in composition and calc-alkaline in character, while intrusive rocks (stocks and small plutons) are granodioritic and dioritic in composition. New zircon U–Pb laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) dating yielded ages from 72.49 ± 0.79 (Upper Cretaceous–Campanian) to 65.44 ± 0.93 Ma (Lower Paleocene–Danian) for the intermediate dykes, and 58.9 ±...
- absolute age
- alkaline earth metals
- Asia
- Black Sea
- Cenozoic
- composition
- Cretaceous
- crystallization
- dikes
- East Mediterranean
- emplacement
- genesis
- geochemistry
- geodynamics
- ICP mass spectra
- igneous rocks
- intrusions
- isotope ratios
- isotopes
- Istanbul Turkey
- laser ablation
- laser methods
- mafic composition
- magmas
- magmatism
- mantle
- mass spectra
- Mediterranean Sea
- melts
- Mesozoic
- metals
- Middle East
- Nd-144/Nd-143
- neodymium
- ocean basins
- Paleocene
- Paleogene
- Paleozoic
- petrography
- plate tectonics
- rare earths
- spectra
- Sr-87/Sr-86
- stable isotopes
- stocks
- strontium
- Tertiary
- thermal properties
- Turkey
- U/Pb
- Upper Cretaceous
- volcanic rocks
- whole rock