PECULIARITIES OF CHEMICAL COMPOSITION OF SKELETAL REMAINS OF CORAL FROM MIDDLE AND UPPER CARBONIFEROUS SEDIMENTS OF THE DONETS BASIN

2016 ◽  
pp. 41-46
Author(s):  
O. Bakhtarova ◽  
◽  
A. Pryvalov ◽  
Keyword(s):  
Chemical Composition ◽  
Skeletal Remains ◽  
Donets Basin ◽  
Upper Carboniferous

An Integrated Approach to Well Logging: The Case of the Bazhenov Formation

2021 ◽  
Author(s):  
Dmitry Mikhailovich Lazutkin ◽  
Oleg Vladimirovich Bukov ◽  
Denis Vagizovich Kashapov ◽  
Albina Viktorovna Drobot ◽  
Maria Alexandrovna Stepanova ◽  
...  
Keyword(s):  
Gulf Of Mexico ◽  
Integrated Approach ◽  
Donets Basin ◽  
Lower Carboniferous ◽  
Upper Carboniferous ◽  
Salt Domes ◽  
Axial Part ◽  
Gravity And Magnetic ◽  
Play Elements ◽  
Hydrocarbon Reserves

Abstract New geological structures – displaced blocks of salt diapirs’ overburden – were identified in the axial part of the Dnieper-Donets basin (DDB) beside one of the largest salt domes due to modern high-precision gravity and magnetic surveys and their joint 3D inversion with seismic and well log data. Superposition of gravity lineaments and wells penetrating Middle and Lower Carboniferous below Permian and Upper Carboniferous sediments in proximity to salt allowed to propose halokinetic model salt overburden displacement, assuming Upper Carboniferous reactivation. Analogy with rafts and carapaces of the Gulf of Mexico is considered in terms of magnitude of salt-induced deformations. Density of Carboniferous rocks within the displaced flaps evidence a high probability of hydrocarbon saturation. Possible traps include uplifted parts of the overturned flaps, abutting Upper Carboniferous reservoirs, and underlying Carboniferous sequence. Play elements are analyzed using analogues from the Dnieper-Donets basin and the Gulf of Mexico. Hydrocarbon reserves of the overturned flaps within the study area are estimated to exceed Q50 (Р50) = 150 million cubic meters of oil equivalent.

Discussion on high-precision 40Ar/39Ar spectrum dating on sanidine from the Donets Basin, Ukraine: evidence for correlation problems in the Upper Carboniferous

2001 ◽  
Vol 158 (4) ◽  
pp. 733-736 ◽  
Author(s):  
MANFRED MENNING ◽  
DIETER WEYER ◽  
IMMO WENDT ◽  
NICHOLAS J. RILEY ◽  
VLADIMIR I. DAVYDOV
Keyword(s):  
High Precision ◽  
Donets Basin ◽  
Upper Carboniferous

The chemical composition of Upper Carboniferous pteridosperm cuticles

1994 ◽  
Vol 21 (1) ◽  
pp. 107-112 ◽  
Author(s):  
Pim F. van Bergen ◽  
Andrew C. Scott ◽  
Patrick J. Barrie ◽  
Jan W. de Leeuw ◽  
Margaret E. Collinson
Keyword(s):  
Chemical Composition ◽  
Upper Carboniferous

Carapaces of the Dnieper-Donets Basin as a New Exploration Target

2021 ◽  
Author(s):  
Tetiana Petrovska ◽  
Oleksandr Petrovskyy ◽  
Oksana Tsihovska ◽  
Andrii Trachuk
Keyword(s):  
Gulf Of Mexico ◽  
Donets Basin ◽  
Well Log ◽  
Lower Carboniferous ◽  
Upper Carboniferous ◽  
Salt Domes ◽  
Axial Part ◽  
Gravity And Magnetic ◽  
Play Elements ◽  
Hydrocarbon Reserves

Abstract New geological structures - displaced blocks of salt diapirs’ overburden - were identified in the axial part of the Dnieper-Donets basin (DDB) beside one of the largest salt domes due to modern high-precision gravity and magnetic surveys and their joint 3D inversion with seismic and well log data. Superposition of gravity lineaments and wells penetrating Middle and Lower Carboniferous below Permian and Upper Carboniferous sediments in proximity to salt allowed to propose halokinetic model salt overburden displacement, assuming Upper Carboniferous reactivation. Analogy with rafts and carapaces of the Gulf of Mexico is considered in terms of magnitude of salt- induced deformations. Density of Carboniferous rocks within the displaced flaps evidence a high probability of hydrocarbon saturation. Possible traps include uplifted parts of the overturned flaps, abutting Upper Carboniferous reservoirs, and underlying Carboniferous sequence. Play elements are analyzed using analogues from the Dnieper-Donets basin and the Gulf of Mexico. Hydrocarbon reserves of the overturned flaps within the study area are estimated to exceed Q50 (P50) = 150 million cubic meters of oil equivalent.

Assemblage Data and Bone and Teeth Modifications as an Aid to Paleoenvironmental Interpretations of the Open-Air Pleistocene Site of Tighenif (Algeria)

1994 ◽  
Vol 42 (3) ◽  
pp. 340-349 ◽  
Author(s):  
Yannicke Dauphin ◽  
Casimir Kowalski ◽  
Christiane Denys
Keyword(s):  
Chemical Composition ◽  
Fossil Record ◽  
Climatic Changes ◽  
Skeletal Remains ◽  
Complex Interaction ◽  
Fossil Bones

AbstractVariations in the proportions of the various groups of Rodentia collected from eight stratigraphic levels at Tighenif had previously been interpreted as representing environmental (climatic) changes. However, the processes involved in the formation of assemblages are still not well understood. Examination of fragmentation, crystallinity, and chemical composition of fossil bones and teeth, compared to recent samples, shows that a possible explanation for the variations in frequencies is the differential preservation of skeletal remains. Thus, the evaluation of postmortem effects is essential in determining the accuracy of the fossil record. The abundance and composition of remains are governed by the complex interaction of many factors. As indicated by actualistic studies, direct deductions from fauna lists must be avoided as much as possible.

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