標(biāo)題: Titlebook: Generation, Accumulation and Production of Europe’s Hydrocarbons III; Special Publication Anthony M. Spencer Conference proceedings 1993 S [打印本頁] 作者: Destruct 時間: 2025-3-21 16:45
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書目名稱Generation, Accumulation and Production of Europe’s Hydrocarbons III讀者反饋學(xué)科排名
作者: FOIL 時間: 2025-3-21 23:31
Upper Jurassic Deep-Water Heterogeneous Reservoirs in the Thelma Fields, UK North Seaurbidite deposits. The porosity network, studied by image analysis, is characterized by secondary pores connected by large throats. A minor percentage of authigenic illite in the water zone dramatically reduces the permeability..Radiometric dating and isotopic analysis allow the diagenetic events to作者: heart-murmur 時間: 2025-3-22 03:05
Enhancing the Oil Potential of Secondary Triassic Reservoirs in the Beryl A Field, UK North Seaificant additional potential resources exist in downthrown terraces to the east. Formation lithologies are interbedded lacustrine shales and finegrained sheet sands with extensive calcrete horizons. Porosity and permeability values range from 10–16% and 10–200 mD, becoming poorer in the eastern terr作者: Moderate 時間: 2025-3-22 08:33
Multi-Disciplinary Stratigraphic Analysis of the Upper Jurassic Strata of the Norwegian Central Troully controlled flooding event of Late Kimmeridgian age (. ammonite zone) marks the base of Sequence B. Different sedimentary facies within this sequence constitute rich hydrocarbon source-rock shales in the Feda Graben and important reservoir sandstones on the Cod Terrace. The Sequence B/C1 transiti作者: 煤渣 時間: 2025-3-22 10:33
Salt Controls on Basin Evolution — Central North Searetaceous thermal subsidence in the North Sea was enhanced in the region of the salt basin by the development of major salt withdrawal synclines which acted as important sediment sinks during the Early Cretaceous. This episode of halokinesis in the basin, focusing on the main areas of Late Jurassic 作者: Infusion 時間: 2025-3-22 13:17
Neogene Uplift and Erosion Offshore South Norway: Magnitude and Consequences for Hydrocarbon Exploraon the northern margin of the Norwegian-Danish Basin. It is a frontier area expected to be opened for exploration within the next few years. The consequences of the uplift for the prospectivity of the Farsund Basin are illustrated, assuming the existence of a Jurassic source rock there. At its prese作者: Infusion 時間: 2025-3-22 19:27 作者: Ostrich 時間: 2025-3-22 23:10 作者: 符合規(guī)定 時間: 2025-3-23 04:14 作者: 樣式 時間: 2025-3-23 06:47
The Petroleum System in the Lower Saxony Basin the nearby source rocks. The bulk of the traps originated during the inversion phase in Santonian times..Present-day maturities of the source rocks indicate an oil window between 0.5 and 0.85% Rr for the Posidonia shale and between 0.45 and 0.8% Rr for the “Wealden” shales. More highly mature sourc作者: 擴張 時間: 2025-3-23 11:32 作者: Biomarker 時間: 2025-3-23 15:10
Organic Geochemistry and Depositional Environment of a Hydrocarbon Source Rock: The Middle Triassic the primary organic matter production in the basin. Variations in the maturity-dependent Ts/Tm ratio and 20S/20R C29 sterane isomerization ratio occur over thicknesses of a few metres. Their correlation with the carbon isotope composition of the extracts suggests that the scatter may be related to 作者: Missile 時間: 2025-3-23 22:00 作者: adulterant 時間: 2025-3-23 22:28 作者: moribund 時間: 2025-3-24 06:09
Generation, Accumulation and Production of Europe’s Hydrocarbons IIISpecial Publication 作者: MEET 時間: 2025-3-24 07:10
Special Publication of the European Association of Petroleum Geoscientists382298.jpg作者: ineluctable 時間: 2025-3-24 11:31 作者: Redundant 時間: 2025-3-24 18:41 作者: EVEN 時間: 2025-3-24 21:41
Joint R&D and Industrial Policy in Japanurbidite deposits. The porosity network, studied by image analysis, is characterized by secondary pores connected by large throats. A minor percentage of authigenic illite in the water zone dramatically reduces the permeability..Radiometric dating and isotopic analysis allow the diagenetic events to作者: 下船 時間: 2025-3-25 01:10
Theoretical Foundation and Related Research,ificant additional potential resources exist in downthrown terraces to the east. Formation lithologies are interbedded lacustrine shales and finegrained sheet sands with extensive calcrete horizons. Porosity and permeability values range from 10–16% and 10–200 mD, becoming poorer in the eastern terr作者: deriver 時間: 2025-3-25 04:33
Missile Defense and the Asian Cascade,lly controlled flooding event of Late Kimmeridgian age (. ammonite zone) marks the base of Sequence B. Different sedimentary facies within this sequence constitute rich hydrocarbon source-rock shales in the Feda Graben and important reservoir sandstones on the Cod Terrace. The Sequence B/C1 transiti作者: nascent 時間: 2025-3-25 09:50 作者: 撤退 時間: 2025-3-25 12:11
D. Rajasekhar,R. Manjula,T. Paranjothion the northern margin of the Norwegian-Danish Basin. It is a frontier area expected to be opened for exploration within the next few years. The consequences of the uplift for the prospectivity of the Farsund Basin are illustrated, assuming the existence of a Jurassic source rock there. At its prese作者: 歸功于 時間: 2025-3-25 18:40 作者: APEX 時間: 2025-3-25 20:58 作者: Pamphlet 時間: 2025-3-26 03:41
,Ann?herung an den Untersuchungsgegenstand, the seismic reflection attributes of siltstones or shales, are frequently cut by upper fan channellized sand-prone strata. Drilling results from the basin confirm the presence of lithofacies ranging from channellized conglomerates and sandstones to turbiditic siltstones and mudstones..The Upper Jur作者: Amylase 時間: 2025-3-26 06:57 作者: LEERY 時間: 2025-3-26 11:02
https://doi.org/10.1007/1-4020-4075-Xlts are listric and flatten out at base Tertiary level or within the Chalk. Some were already active around the end Cretaceous times, but most are Oligocene-Miocene in age, i.e. they have the same age as the dome. The radial fault pattern is characteristic of salt-induced circular domes and can be e作者: hauteur 時間: 2025-3-26 13:14
Stanley Kirschner (Professor of Chemistry) the primary organic matter production in the basin. Variations in the maturity-dependent Ts/Tm ratio and 20S/20R C29 sterane isomerization ratio occur over thicknesses of a few metres. Their correlation with the carbon isotope composition of the extracts suggests that the scatter may be related to 作者: cutlery 時間: 2025-3-26 16:55
What Are Organometallic Compounds?,op..The basal Maastrichtian unit consists of thick, laterally continuous, relatively fine-grained turbidite beds, sometimes separated by thin micritic partings, with well-developed normal grading and laminations..The upper Maastrichtian-Palaeocene unit consists of very coarsegrained turbidites chara作者: Campaign 時間: 2025-3-26 21:00
Proton-containing Acceptor Solvents,itudinal joints, sub parallel to the axial trend, and diagonal joints, oblique to the axial trend, are also present although less abundant. The latter are usually associated with zones of strike-slip deformation. Bedding joints are very rare..The overall characteristics of the analyzed jointing are 作者: 用不完 時間: 2025-3-27 02:36 作者: neutralize 時間: 2025-3-27 08:02 作者: apiary 時間: 2025-3-27 13:04 作者: 規(guī)范要多 時間: 2025-3-27 14:23 作者: 該得 時間: 2025-3-27 19:48
https://doi.org/10.1007/978-1-4614-4388-9nd muds underlain by 123 m of homogeneous, structureless sands. A conventional depositional model suggested that this stratigraphy was the result of turbidite deposition on a retreating submarine fan. A fundamental problem arose in that the sand envelope defined on seismic data suggested a confined 作者: legislate 時間: 2025-3-27 23:02
Joint R&D and Industrial Policy in Japan Thelma oil fields. They lie on the western margin of the South Viking Graben and are combined structural/stratigraphic traps. The Ryazanian-Late Callovian strata are subdivided into 11 palynologic units, comprising three sequences bounded by major hiatuses. These correspond to major basin-modifying作者: 羊齒 時間: 2025-3-28 05:02 作者: 含水層 時間: 2025-3-28 07:10
Missile Defense and the Asian Cascade,rassic times, the area was split into structural elements by several phases of tectonic movement. In both shallow- and deep-water environments the sedimentary response to tectonic episodes occurred simultaneously, but differed in lithology and intensity, resulting in a highly varied facies developme作者: 節(jié)省 時間: 2025-3-28 12:24
https://doi.org/10.1007/978-981-13-8359-5nics and sedimentation in the area throughout the Mesozoic and Tertiary..The salt accumulated in the northernmost of two Zechstein basins lying north of the east-west trending Variscan mountain front. Salt withdrawal and dissolution during the Triassic and Early/mid-Jurassic led to the formation of 作者: 施舍 時間: 2025-3-28 17:15
Fundamentals of Matching Theory,eometry and its rollover structure through Tertiary time. Contour displacement diagrams on a vertical plane parallel to the fault strike and vertical displacement maps of the lateral displacement distribution have been produced for different times in the Tertiary. The distortion of the regular semi-作者: Highbrow 時間: 2025-3-28 20:06
D. Rajasekhar,R. Manjula,T. Paranjothi Fennoscandian Shield. Using vitrinite reflectance trends, shale compaction and reconstructed regional seismic profiles, we have quantified and mapped the regional uplift of the strata underlying the Base Quaternary unconformity. There is no erosion in the Central Graben area of the North Sea, but f作者: 愛社交 時間: 2025-3-28 23:30 作者: Fulminate 時間: 2025-3-29 05:53
Large Linear Systems of Binding Sites, been licensed for exploration. Sampling for surface geochemistry has been undertaken using a gravity corer, where samples were taken 2 m below the seafloor. The sampling grids were either regular or irregular based on known geological features in the areas, or a combination of the two. The samples 作者: MURKY 時間: 2025-3-29 10:24 作者: avulsion 時間: 2025-3-29 14:30
Core Books in Advanced Mathematicsied out on the structural and maturity development, source rocks, and hydrocarbons in 67 hydrocarbon fields within the Lower Saxony Basin, NW Germany. The hydrocarbons were generated from two source rocks, the Liassic Posidonia shale and the “Wealden” bituminous shales of Ryazanian age (occurring ex作者: entail 時間: 2025-3-29 15:34
https://doi.org/10.1007/1-4020-4075-Xdome. Halokinesis of the Zechstein salt started in Late Triassic times. The salt diapir formed in Late Jurassic to Early Cretaceous times. The dome in the Chalk overburden, however, was formed mainly during Late Cretaceous and Oligocene-Miocene times by late movement of the salt..A detailed structur作者: IST 時間: 2025-3-29 21:20 作者: Rustproof 時間: 2025-3-30 02:22
Stanley Kirschner (Professor of Chemistry)ch 10% in the dolomites and 40% in the shales. Sedimentological and geochemical data suggest deposition in a shallow marine basin under permanently anoxic conditions. The organic matter is of type II. Based on geochemical parameters the Grenzbitumenzone can be divided into two sections. In the lower作者: 長處 時間: 2025-3-30 06:38 作者: Parabola 時間: 2025-3-30 11:44 作者: Armada 時間: 2025-3-30 14:44 作者: 控制 時間: 2025-3-30 16:59
Fundamentals of Matching Theory,effects on the development of the fault geometry, causing a shift from a concave to a convex upwards geometry in Late Tertiary times. The change in fault curvature has produced a rollover structure in the hangingwall, a likely site for hydrocarbon accumulation.作者: EXCEL 時間: 2025-3-31 00:01 作者: Legend 時間: 2025-3-31 01:53
Evolution of a Salt-Related Tertiary Growth Fault in the Danish North Seaeffects on the development of the fault geometry, causing a shift from a concave to a convex upwards geometry in Late Tertiary times. The change in fault curvature has produced a rollover structure in the hangingwall, a likely site for hydrocarbon accumulation.作者: crutch 時間: 2025-3-31 05:15 作者: 追蹤 時間: 2025-3-31 09:37
al and eastern Mediterranean including offshore Albania, central and eastern Europe including Poland, Hungary, the Russian platform and offshore Bulgaria. Main topics are investigations to sequence stratigraphy, 3D-quantitative restoration and balanced structural sections, using the LOCACE equipment作者: HACK 時間: 2025-3-31 14:58 作者: SPASM 時間: 2025-3-31 18:38 作者: GEM 時間: 2025-3-31 22:24
