Results 141 to 150 of about 348 (177)
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Quantitative estimation of overpressure caused by oil generation in petroliferous basins
Organic Geochemistry, 2011Abstract Oil generation can be the dominant overpressure mechanism in low permeability source rocks because of the volume increase upon conversion of organic matter to less dense oil during the petroleum generation process. To quantitatively express the relationship between oil generation and overpressure in source rocks, an equation for the pressure
Xiaowen Guo +3 more
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Fluidodynamics in Deep Formations of the Eastern Ciscaucasia Petroliferous Basin
2009The geological, hydrogeological, and tectonic settings of the eastern Ciscaucasia petroliferous basin are described in [4, 8]. Figure 9.1 presents the schematic geological and tectonic structure of the basin (Terek-Sunzha area included).
V.I. Djunin, A.V. Korzun
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Principal Formation Model of Deep Fluids in Petroliferous Basins
2009The main peculiarities in the formation of deep subsurface fluids in artesian basins of platform demonstrate that (1) peripheral parts of petroliferous basins (“regional recharge areas”) provide no influence on the formation of deep fluid in the zone of very slow water exchange ( Chapter 7, Chapter 9, and Chapter 10); (2 ...
V.I. Djunin, A.V. Korzun
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Character of Ancient Petroliferous Lake Basins of the World: ABSTRACT
AAPG Bulletin, 1982The principal oil- and gas-bearing lacustrine rocks in the world were formed from sediments deposited in or peripheral to ancient stratified lakes, of a variety of ages, which for millions of years maintained a size comparable to that of modern inland seas. In these lake systems, both lipid and woody organic matter were developed and preserved in large
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Small-scale petroliferous basins in China: Characteristics and hydrocarbon occurrence
AAPG Bulletin, 2019ABSTRACT A large number of small-scale lacustrine sedimentary basins are widely distributed across China. Studies of such basins have been limited. These basins have complex characteristics and thus exhibit significant differences in terms of their hydrocarbon potential.
Chi-yang Liu +8 more
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Development of Filtration Properties in Deep Formations of Petroliferous Basins
2009The regional aspects concerning capacity and filtration properties are least studied among others in the general problem of deep fluid formation in stratified systems of negative structures. They are poorly covered in special works dedicated to the formation of deep fluids. Practically all the available information on capacity and filtration properties
V.I. Djunin, A.V. Korzun
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Geologic Evolution of Petroliferous Basins on Continental Shelf of China
AAPG Bulletin, 1984ABSTRACT The coastline of southeastern China is about 18,000 km (11,200 mi) in length, and its aggregate continental shelf area within 200-m (660-ft) water depth is well over 1 million km2 (390,000 mi2). Recent geophysical exploration and petroleum drilling records aid in understanding the geologic evolution of these petroliferous ...
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Structure and geological history of sedimentary petroliferous basins in the North Atlantic
Lithology and Mineral Resources, 2009Pericontinental sedimentary basins in the northern Atlantic Ocean contain the largest reserves of oil and gas. In the Paleozoic-initial Paleogene period, they were developing as rift grabens subjected to repeated tectonic dislocations. Spreading of the oceanic bottom that started in this region in the Paleocene-Eocene was accompanied by rapid ...
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Fluidodynamics in Hydrocarbon-Bearing Formations of the Northern Pechora Petroliferous Basin
2009We consider here only the northern part of the Pechora petroliferous basin belonging to the Timan-Pechora Province. The basin is bordered by the Kolva Megaswell, Sorokin Swell, Pechora Sea, and Chernyshev Range in the west, east, north, and south, respectively.
V.I. Djunin, A.V. Korzun
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Structural Styles of Mesozoic-Cenozoic Petroliferous Basins of China: ABSTRACT
AAPG Bulletin, 1982The continental lithosphere of China is situated at the junction of the Marginal Pacific tectonic domain and the Tethys-Himalayan tectonic domain. The former is characterized by a series of extensional tectonics, including taphrogenesis and the latter by a series of compressional tectonics with orogenesis, all taking place during the Mesozoic and ...
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