Results 211 to 220 of about 1,161,013 (254)
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Gravitationally Induced Non-karst Caves in the Polish Outer Carpathians

World Geomorphological Landscapes
Jan Urban, Wlodzimierz Margielewski
exaly   +2 more sources

A New Saturated and Aromatic Hydrocarbon‐Based Scheme to Decipher the Origin of Extracted Organic Matter in the Outer Carpathians: From the Jurassic to the Miocene

Journal of Petroleum Geology
In this review, published and new geochemical data characterising 17 potential source rocks for hydrocarbons in the Polish part of the Outer Carpathians have been used to establish a new scheme that can be useful for oil–source rock correlations.
Mirosław Słowakiewicz
semanticscholar   +1 more source

Organic Matter Thermal Maturity Versus Variability of the Present‐Day Thermal Gradient of the Eastern Part of Polish Outer Carpathians—The Key to the Success or Failure of Hydrocarbon Generation Processes

Journal of Petroleum Geology
This study presents an integrated analysis of organic matter (OM) maturity proxies, including Rock‐Eval pyrolysis, vitrinite reflectance, and the spore color standard (SCS), in conjunction with a pre‐existing 3D numerical model of the present‐day ...
Anna Filipek   +9 more
semanticscholar   +1 more source

Palynofacies Analysis Illustrates the Source Rock Potential of the Menilite Beds, Polish Outer Carpathians

Journal of Petroleum Geology
The deposition of the Menilite Beds began during the reorganization of the sea ways and the extensional stage of the Carpathian Basin evolution in the early Oligocene.
Anna Filipek   +3 more
semanticscholar   +1 more source

Reinterpretation of geological data as to the tectonics of separate covers and subcovers of the Outer Carpathians (in the context of prospects for oil and gas presence)

Geology and Geochemistry of Combustible Minerals
In spite of a number of preliminary investigations, the Ukrainian portion of the Outer Carpathians continues to be the object for scientific discussions of the modern geologists.
V. Shlapinsky   +3 more
semanticscholar   +1 more source

The Eocene Spiroplectammina spectabilis Acme in the Outer Carpathians

Micropaleontology
The subject of this study are deep water agglutinated assemblages with an increased abundance of Spiroplectammina spectabilis (Grzybowski) and their biostratigraphic utility. Qualitative and quantitative observations of foraminiferal assemblages indicate that, in the Outer Carpathians, Spiroplectammina spectabilis acme assemblages occur within a ...
Anna Waskowska   +3 more
openaire   +1 more source

Origin, secondary processes and migration of oil and natural gas in the central part of the Polish Outer Carpathians

, 2020
The origin, migration pathways, and the influence of secondary processes of oil and natural gas accumulated in Lower Cretaceous to Lower Miocene strata of the central part of the Polish Outer Carpathians are investigated based on organic geochemical ...
M. Kotarba   +7 more
semanticscholar   +1 more source

Outline of tectonics of the outer zone, the Carpathian foretrough

International Geology Review, 1965
The edge trough in the East Carpathians includes an inner zone that developed adjacent to the Carpathian geosyncline, a deep trough filled with thick Miocene and Pliocene sediments. The Miocene beds have been extensively folded and overthrust. The edge trough also includes an outer zone which is the depressed edge of the platform covered by Tortonian ...
openaire   +1 more source

Reconstruction of landslide movements using Digital Elevation Model and Electrical Resistivity Tomography analysis in the Polish Outer Carpathians

, 2020
Landslides are a major threat to the environment, infrastructure and human activities, especially in mountainous and hilly areas. It is therefore important to accurately identify the mass movements triggering these mechanisms.
Jarosław Cebulski   +3 more
semanticscholar   +1 more source

Geologically controlled waterfall types in the Outer Carpathians

Geomorphology, 1994
Abstract More then fourty waterfalls occurring in the Polish Outer Carpathians have been studied with regard to their geological settings. They are small forms developed on faulted flysch rocks of different resistance on streams characterized by similar features of catchment basins and similar discharges.
openaire   +1 more source

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