Results 171 to 180 of about 601 (207)
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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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Heat and Mass Transfer in Deep Formations of Petroliferous Basins
2009Both lateral and vertical deep fluid hydrodynamics are irregularly studied; the available data concern largely productive formations, while the remainder of the section remains unknown or poorly known with respect to its hydrogeology. Therefore, the vertical distribution of formation pressures and filtration properties is insufficiently studied.
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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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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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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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, Djunin V I
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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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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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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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Geological structure, evolution stages, and petroliferous complexes of the Gulf of Mexico basin
Lithology and Mineral Resources, 2008The Gulf of Mexico basin occupies a vast region encompassing the southern continental margin of North America, a considerable part of the Greater Antilles, and the intervening Sigsbee Deep with the oceanic crust. In the north, the basin is contiguous with spurs of the Hercynian Appalachians, the Mississippi Interior and Permian basins.
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