Results 161 to 170 of about 601 (207)

Petroliferous basins at continental margins of Paleozoic paleoseas: Communication 1. Petroliferous basins at margins of Iapetus and Panthalassa

Lithology and Mineral Resources, 2013
Although large marine basins governing the fabric of our planet in the Paleozoic disappeared later (whether or not they were oceans is a debatable issue), sedimentary basins formed at continental margins at that time played a crucial role as depositories of various fossil minerals, including ores, salts, phosphorites, coal, bauxites, and construction ...
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Hydrocarbon occurrences in the petroliferous basins of western China

Marine and Petroleum Geology, 1995
Abstract The compressional basins of western China result from the stress caused by the northward collision of the Indian plate. Most of the large intracratonic basins between the fold belts have undergone a long history of differentiation and superposition that has resulted in the prolific oil and gas reserves of the Tarim, Junggar and Qaidam basins.
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Fluidodynamics in Deep Formations of the Bukhara–Karshi Petroliferous Basin

2009
The second-order Bukhara–Karshi petroliferous basin represents an element of the more complex Amudar’ya (Karakumy) basin. It consists of the Paleozoic basement and Mesozoic–Cenozoic sedimentary cover. Figure 10.1 yields some ideas about the geological structure and tectonics of the basin.
V I Djunin, A V Korzun, Djunin V I
exaly   +2 more sources

Fluidodynamics in Deep Formations of the West Siberian Petroliferous Basin

2009
The geological structure, general hydrogeological conditions, and tectonics of this petroliferous basin are discussed in numerous publications. Therefore, we present only the data necessary for solving the main task of this study: interpretation of hydrodynamics in deep formations.
V I Djunin, A V Korzun, Djunin V I
exaly   +2 more sources

Computer simulations for estimation of petroliferous potential of sedimentary basins

EAEG/EAPG/EAGO Joint Multidisciplinary Workshop - Developing New Reservoirs in Europe, 1994
The topic under discussion is mathematical models and computer techniques developed at VNIGRI for simulation of reaI exploration process which provide basis for sound strategie decisions of future oil and gas exploration efforts. Decisions are based on the results of multivariant geo-economic analyses, comparisons and their conformity to certain ...
M. D. Belonn, Y. V. Podolsky
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Fluidodynamics in Deep Formations of the Eastern Ciscaucasia Petroliferous Basin

2009
The 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, Djunin V I
exaly   +2 more sources

Pericontinental petroliferous basins of the South Atlantic Ocean

Lithology and Mineral Resources, 2008
Sedimentary basins located at Atlantic margins of South America and Africa (Brazil, Congo, and Angola) are composed of thick Cretaceous-Pleistocene rocks (7–9 km). The principal oil-bearing complexes of both regions are dominated by terrigenous rocks.
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EFFICIENCY OF PETROLEUM CONCENTRATION IN MAJOR PETROLIFEROUS BASINS

Journal of Petroleum Geology, 1992
The ratio of the concentration (barrels of oil equivalent/sq. km) of accumulated oil in the richest sedimentary basin to that in the poorest basin, among those basins containing “giant” and “super‐giant” fields, is more than 500 to 1. By contrast, the ratio of the richest to the poorest petroliferous basin in terms of average organic concentration may ...
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PROSPECTIVE PETROLIFEROUS AREAS IN THE EAST CHINA SEA BASIN

Journal of Petroleum Geology, 1990
The East China Sea Basin is a major Cenozoic basin, with a sedimentary fill greater than 10,000 metres in thickness. The evolution of the basin is divisible into four stages‐down‐faulting, fault‐sagging, down‐warping and draping. Tectonic movements were characterized by multiple episodes of spatial differentiation, and tectonic units are divisible into
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Petroliferous basins at continental margins of paleozoic paleoseas: Communication 2. Petroliferous basins at continental margins in the Rheic, Uralian, and Central Asian paleoseas

Lithology and Mineral Resources, 2013
The continental block of the Earth’s crust was separated in the Paleozoic into two unequal parts: (i) huge supercontinent Gondwana located at high latitudes of the Southern Hemisphere and (ii) several small continents (Laurentia, Baltica, Siberia, Kazakhstan, South Chinese block, and North Chinese blocks) located at low latitudes south and north of the
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