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  • 1
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    Deltas : Sites and Traps for Fossil Fuels (1989)
    Oxford, London, Edinburgh, Boston, Melbourne : Blackwell Scientific Publications
    Details
    Keywords: Delta ; Deltasediment ; Erdölgeologie ; Combustibles fossiles ; Deltas ; Pétrole - Géologie ; Sedimentation and deposition ; Sédimentation (géologie) ; Sédiments (géologie) ; Traps (Petroleum geology)
    Description / Table of Contents: Deltaic Systems and General Models --- T. Elliott: Deltaic systems and their contribution to an understanding of basin-fill successions / Geological Society, London, Special Publications, 41:3-10, doi:10.1144/GSL.SP.1989.041.01.01 --- J. Alexander: Delta or coastal plain? With an example of the controversy from the Middle Jurassic of Yorkshire / Geological Society, London, Special Publications, 41:11-19, doi:10.1144/GSL.SP.1989.041.01.02 --- J. P. M. Syvitski and G. E. Farrow: Fjord sedimentation as an analogue for small hydrocarbon-bearing fan deltas / Geological Society, London, Special Publications, 41:21-43, doi:10.1144/GSL.SP.1989.041.01.03 --- M. Ito: Profiles of fan deltas and water depth in the receiving basin / Geological Society, London, Special Publications, 41:45-54, doi:10.1144/GSL.SP.1989.041.01.04 --- Subsurface and Geophysical Techniques --- G. Cowan: Diagenesis of Upper Carboniferous sandstones: southern North Sea Basin / Geological Society, London, Special Publications, 41:57-73, doi:10.1144/GSL.SP.1989.041.01.05 --- C. S. Bristow and K. J. Myers: Detailed sedimentology and gamma-ray log characteristics of a Namurian deltaic succession I: Sedimentology and facies analysis / Geological Society, London, Special Publications, 41:75-80, doi:10.1144/GSL.SP.1989.041.01.06 --- K. J. Myers and C. S. Bristow: Detailed sedimentology and gamma-ray log characteristics of a Namurian deltaic succession II: Gamma-ray logging / Geological Society, London, Special Publications, 41:81-88, doi:10.1144/GSL.SP.1989.041.01.07 --- R. C. Selley: Deltaic reservoir prediction from rotational dipmeter patterns / Geological Society, London, Special Publications, 41:89-95, doi:10.1144/GSL.SP.1989.041.01.08 --- Selected Delta Case Studies --- G. Sestini: Nile Delta: a review of depositional environments and geological history / Geological Society, London, Special Publications, 41:99-127, doi:10.1144/GSL.SP.1989.041.01.09 --- H. Okazaki and F. Masuda: Arcuate and bird’s foot deltas in the late Pleistocene Palaeo-Tokyo Bay / Geological Society, London, Special Publications, 41:129-138, doi:10.1144/GSL.SP.1989.041.01.10 --- G. K. Pedersen: A fluvial-dominated lacustrine delta in a volcanic province, W Greenland / Geological Society, London, Special Publications, 41:139-146, doi:10.1144/GSL.SP.1989.041.01.11 --- J. P. Harris: The sedimentology of a Middle Jurassic lagoonal delta system: Elgol Formation (Great Estuarine Group), NW Scotland / Geological Society, London, Special Publications, 41:147-166, doi:10.1144/GSL.SP.1989.041.01.12 --- O. J. Martinsen: Styles of soft-sediment deformation on a Namurian (Carboniferous) delta slope, Western Irish Namurian Basin, Ireland / Geological Society, London, Special Publications, 41:167-177, doi:10.1144/GSL.SP.1989.041.01.13 --- A. J. Pulham: Controls on internal structure and architecture of sandstone bodies within Upper Carboniferous fluvial-dominated deltas, County Clare, western Ireland / Geological Society, London, Special Publications, 41:179-203, doi:10.1144/GSL.SP.1989.041.01.14 --- A. Siedlecka, K. T. Pickering, and M. B. Edwards: Upper Proterozoic passive margin deltaic complex, Finnmark, N Norway / Geological Society, London, Special Publications, 41:205-219, doi:10.1144/GSL.SP.1989.041.01.15 --- Petroleum- and Gas-related Case Histories --- S. Flint, D. J. Stewart, and E. D. van Riessen: Reservoir geology of the Sirikit oilfield, Thailand: lacustrine deltaic sedimentation in a Tertiary intermontane basin / Geological Society, London, Special Publications, 41:223-235, doi:10.1144/GSL.SP.1989.041.01.16 --- W. Helland-Hansen, R. Steel, K. Nakayama, and C. G. St. C. Kendall: Review and computer modelling of the Brent Group stratigraphy / Geological Society, London, Special Publications, 41:237-252, doi:10.1144/GSL.SP.1989.041.01.17 --- S. Brown and P. C. Richards: Facies and development of the Middle Jurassic Brent Delta near the northern limit of its progradation, UK North Sea / Geological Society, London, Special Publications, 41:253-267, doi:10.1144/GSL.SP.1989.041.01.18 --- S. E. Livera: Facies associations and sand-body geometries in the Ness Formation of the Brent Group, Brent Field / Geological Society, London, Special Publications, 41:269-286, doi:10.1144/GSL.SP.1989.041.01.19 --- Coal-related Case Histories --- R. S. Haszeldine: Coal reviewed: depositional controls, modern analogues and ancient climates / Geological Society, London, Special Publications, 41:289-308, doi:10.1144/GSL.SP.1989.041.01.20 --- A. C. Scott: Deltaic coals: an ecological and palaeobotanical perspective / Geological Society, London, Special Publications, 41:309-316, doi:10.1144/GSL.SP.1989.041.01.21 --- M. K. G. Whateley and G. R. Jordan: Fan-delta-lacustrine sedimentation and coal development in the Tertiary Ombilin Basin, W Sumatra, Indonesia / Geological Society, London, Special Publications, 41:317-332, doi:10.1144/GSL.SP.1989.041.01.22 --- W. A. Read: The influence of basin subsidence and depositional environment on regional patterns of coal thickness within the Namurian fluvio-deltaic sedimentary fill of the Kincardine Basin, Scotland / Geological Society, London, Special Publications, 41:333-344, doi:10.1144/GSL.SP.1989.041.01.23
    Pages: Online-Ressource (IX, 360 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 0632023856
    URL: http://sp.lyellcollection.org/content/41/1
    Language: English
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  • 2
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    The United States' next generation of atmospheric composition and coastal ecosystem measurements : NASA's Geostationary Coastal and Air Pollution Events (GEO-CAPE) Mission (2013)
    American Meteorological Society
    Details
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2012. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Bulletin of the American Meteorological Society 93 (2012): 1547–1566, doi:10.1175/BAMS-D-11-00201.1.
    Description: The Geostationary Coastal and Air Pollution Events (GEO-CAPE) mission was recommended by the National Research Council's (NRC's) Earth Science Decadal Survey to measure tropospheric trace gases and aerosols and coastal ocean phytoplankton, water quality, and biogeochemistry from geostationary orbit, providing continuous observations within the field of view. To fulfill the mandate and address the challenge put forth by the NRC, two GEO-CAPE Science Working Groups (SWGs), representing the atmospheric composition and ocean color disciplines, have developed realistic science objectives using input drawn from several community workshops. The GEO-CAPE mission will take advantage of this revolutionary advance in temporal frequency for both of these disciplines. Multiple observations per day are required to explore the physical, chemical, and dynamical processes that determine tropospheric composition and air quality over spatial scales ranging from urban to continental, and over temporal scales ranging from diurnal to seasonal. Likewise, high-frequency satellite observations are critical to studying and quantifying biological, chemical, and physical processes within the coastal ocean. These observations are to be achieved from a vantage point near 95°–100°W, providing a complete view of North America as well as the adjacent oceans. The SWGs have also endorsed the concept of phased implementation using commercial satellites to reduce mission risk and cost. GEO-CAPE will join the global constellation of geostationary atmospheric chemistry and coastal ocean color sensors planned to be in orbit in the 2020 time frame.
    Description: Funding for GEO-CAPE definition activities is provided by the Earth Science Division of the National Aeronautics and Space Administration.
    Description: 2013-04-01
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 3
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    IODP Expedition 338: NanTroSEIZE Stage 3: NanTroSEIZE plate boundary deep riser 2 (2014)
    In:  Scientific drilling : reports on deep earth sampling and monitoring
    Details
    Publication Date: 2020-02-12
    Description: The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) is designed to investigate fault mechanics and seismogenesis along a subduction megathrust, with objectives that include characterizing fault slip, strain accumulation, fault and wall rock composition, fault architecture, and state variables throughout an active plate boundary system. Integrated Ocean Drilling Program (IODP) Expedition 338 was planned to extend and case riser Hole C0002F from 856 to 3600 meters below the seafloor (m b.s.f.). Riser operations extended the hole to 2005.5 m b.s.f., collecting logging-while-drilling (LWD) and measurement-while-drilling, mud gas, and cuttings data. Results reveal two lithologic units within the inner wedge of the accretionary prism that are separated by a prominent fault zone at ~ 1640 m b.s.f. Due to damage to the riser during unfavorable winds and strong currents, riser operations were suspended, and Hole C0002F left for re-entry during future riser drilling operations. Contingency riserless operations included coring at the forearc basin site (C0002) and at two slope basin sites (C0021 and C0022), and LWD at one input site (C0012) and at three slope basin sites (C0018, C0021 and C0022). Cores and logs from these sites comprehensively characterize the alteration stage of the oceanic basement input to the subduction zone, the early stage of Kumano Basin evolution, gas hydrates in the forearc basin, and recent activity of the shallow megasplay fault zone system and associated submarine landslides.
    Type: info:eu-repo/semantics/article
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  • 4
    Electronic Resource
    Electronic Resource
    Sediment deformation and hydrogeology of the Nankai Trough accretionary prism: Synthesis of shipboard results of ODP Leg 131
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 109 (1992), S. 431-450 
    Details
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
    URL: http://linkinghub.elsevier.com/retrieve/pii/0012-821X(92)90104-4
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    Paper (German National Licenses)
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  • 5
    Electronic Resource
    Electronic Resource
    Possible retrogressive flow slide deposits from the Kongsfjord Formation: a Precambrian submarine fan, Finnmark, N. Norway (1979)
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 26 (1979), S. 0 
    Details
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Three thinning and fining-upward turbidite sequences are described from the Precambrian Kongsfjord Formation, a 3.5 km thick flysch succession. Their thicknesses range between about 2 and 5 m. They show a progressive upward decrease in bed thickness, bulk mean grain size and the ratio of the higher to lower energy division of the Bouma sequence. In one case, however, there is an initial upward bed thickness and grain size increase, with an increase in the proportion of the higher energy division. The absence of structureless mud of the Bouma E division and the presence of wavy interfaces between beds, together with similar palaeo-currents within each sequence suggest that these sequences resulted from related depositional events. These sequences are interpreted as the deposits of retrogressive flow slides, as an alternative to the classic mechanism of channel fill after abandonment.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-3091.1979.tb00356.x
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  • 6
    Electronic Resource
    Electronic Resource
    Changes in life cycle characteristics of mammalian cells grown in monolayer culture
    Amsterdam : Elsevier
    Biosystems 1 (1967), S. 165-169 
    Details
    ISSN: 0303-2647
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Biology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1016/0303-2647(67)90048-2
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  • 7
    Electronic Resource
    Electronic Resource
    The shape of deep-water siliciclastic systems: A discussion (1982)
    Springer
    Geo-marine letters 2 (1982), S. 41-46 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Deep-water siliciclastic systems are classified primarily on their shape as: submarine fans with well developed or poorly developed morphology, slope drapes, for example, over relatively stable basin margins, fault-scarp aprons, canyons and large channels, under-supplied sheet systems such as abyssal plains, non-fan ponded systems such as over-supplied perched basins, and fan deltas. Collectively, or separately, these systems may form sedimentary basin fills that can be over or under-supplied with respect to the sediment input although most systems will tend toward over-supply/overflow with time. Finally, the sum total of the siliciclastic systems and basins can be used to define the tectonic milieux such as passive, strike-slip and convergent margins.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02462798
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  • 8
    Electronic Resource
    Electronic Resource
    Reflected turbidity currents on an Ordovician basin floor, Canadian Appalachians (1984)
    [s.l.] : Nature Publishing Group
    Nature 311 (1984), S. 143-145 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The beds form part of the 1.5-km thick ß I and 02 members of the Middle Ordovician Cloridorme Formation6, a flysch unit deposited in a constricted foreland basin during the Taconic Orogeny7. The ß I and 02 sequence consists of thinly-bedded classic turbidites and hemipelagic shales, punctuated ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/311143a0
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  • 9
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    On the origin of pronounced O3 gradients in the thunderstorm outflow region during DC3 (2016)
    Wiley
    Details
    Publication Date: 2016-03-10
    Description: Unique in-situ measurements of CO, O 3 , SO 2 , CH 4 , NO, NO x , NO y , VOC, CN, and rBC were carried out with the German DLR-Falcon aircraft in Central U.S. thunderstorms during the Deep Convective Clouds and Chemistry (DC3) experiment in summer 2012. Fresh and aged anvil outflow (9-12 km) from supercells, mesoscale convective systems, mesoscale convective complexes, and squall lines were probed over Oklahoma, Texas, Colorado, and Kansas. For three case studies (May 30, June 8 and 12) a combination of trace species, radar, lightning, and satellite information, as well as model results, were used to analyze and design schematics of major trace gas transport pathways within and in the vicinity of the probed thunderstorms. The impact of thunderstorms on the O 3 composition in the upper troposphere (UT) / lower stratosphere (LS) region was analyzed. Overshooting cloud tops injected high amounts of biomass burning and lightning-produced NO x emissions into the LS, in addition to low O 3 mixing ratios from the lower troposphere. As a dynamical response, O 3 -rich air from the LS was transported downward into the anvil and also surrounded the outflow. The ΔO 3 /ΔCO ratio was determined in the anvil outflow region. A pronounced in-mixing of O 3 -rich stratospheric air masses was observed in the outflow indicated by highly positive or even negative ΔO 3 /ΔCO ratios (+1.4 down to -3.9). Photochemical O 3 production (ΔO 3 /ΔCO = +0.1) was found to be minor in the recently lofted pollution plumes. O 3 mixing ratios within the aged anvil outflow were mainly enhanced due to dynamical processes.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 10
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    The shape of deep-water siliciclastic systems: A discussion (1982)
    Springer
    Details
    Publication Date: 1982-03-01
    Print ISSN: 0276-0460
    Electronic ISSN: 1432-1157
    Topics: Geosciences
    Published by Springer
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