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  • 1
    Unknown
    London : The Geological Society
    Keywords: Sedimentologie ; Flusssediment ; Flussbett ; Flussmäander ; Fluviale Sedimentation ; Geomorphogenese ; Acao Dos Rios (Geologia) ; Alluvial streams ; Rivieren ; Sediment transport ; Sedimentologia
    Description / Table of Contents: C. S. Bristow and J. L. Best: Braided rivers: perspectives and problems / Geological Society, London, Special Publications, 75:1-11, doi:10.1144/GSL.SP.1993.075.01.01 --- John S. Bridge: The interaction between channel geometry, water flow, sediment transport and deposition in braided rivers / Geological Society, London, Special Publications, 75:13-71, doi:10.1144/GSL.SP.1993.075.01.02 --- R. I. Ferguson: Understanding braiding processes in gravel-bed rivers: progress and unsolved problems / Geological Society, London, Special Publications, 75:73-87, doi:10.1144/GSL.SP.1993.075.01.03 --- N. J. Clifford, J. Hardisty, J. R. French, and S. Hart: Downstream variation in bed material characteristics: a turbulence-controlled form-process feedback mechanism / Geological Society, London, Special Publications, 75:89-104, doi:10.1144/GSL.SP.1993.075.01.04 --- P. F. Friend and R. Sinha: Braiding and meandering parameters / Geological Society, London, Special Publications, 75:105-111, doi:10.1144/GSL.SP.1993.075.01.05 --- M. S. E. Robertson-Rintoul and K. S. Richards: Braided-channel pattern and palaeohydrology using an index of total sinuosity / Geological Society, London, Special Publications, 75:113-118, doi:10.1144/GSL.SP.1993.075.01.06 --- J. O. Leddy, P. J. Ashworth, and J. L. Best: Mechanisms of anabranch avulsion within gravel-bed braided rivers: observations from a scaled physical model / Geological Society, London, Special Publications, 75:119-127, doi:10.1144/GSL.SP.1993.075.01.07 --- Peter Ashmore: Anabranch confluence kinetics and sedimentation processes in gravel-braided streams / Geological Society, London, Special Publications, 75:129-146, doi:10.1144/GSL.SP.1993.075.01.08 --- Christoph Siegenthaler and Peter Huggenberger: Pleistocene Rhine gravel: deposits of a braided river system with dominant pool preservation / Geological Society, London, Special Publications, 75:147-162, doi:10.1144/GSL.SP.1993.075.01.09 --- Peter Huggenberger: Radar facies: recognition of facies patterns and heterogeneities within Pleistocene Rhine gravels, NE Switzerland / Geological Society, London, Special Publications, 75:163-176, doi:10.1144/GSL.SP.1993.075.01.10 --- Peter A. Bentham, Peter J. Talling, and Douglas W. Burbank: Braided stream and flood-plain deposition in a rapidly aggrading basin: the Escanilla formation, Spanish Pyrenees / Geological Society, London, Special Publications, 75:177-194, doi:10.1144/GSL.SP.1993.075.01.11 --- Keith Richards, Shobhit Chandra, and Peter Friend: Avulsive channel systems: characteristics and examples / Geological Society, London, Special Publications, 75:195-203, doi:10.1144/GSL.SP.1993.075.01.12 --- David G. Passmore, Mark G. Macklin, Paul A. Brewer, John Lewin, Barbara T. Rumsby, and Malcolm D. Newson: Variability of late Holocene braiding in Britain / Geological Society, London, Special Publications, 75:205-229, doi:10.1144/GSL.SP.1993.075.01.13 --- David J. Gilvear: River management and conservation issues on formerly braided river systems; the case of the River Tay, Scotland / Geological Society, London, Special Publications, 75:231-240, doi:10.1144/GSL.SP.1993.075.01.14 --- J. Warburton, T. R. H. Davies, and M. G. Mandl: A meso-scale field investigation of channel change and floodplain characteristics in an upland braided gravel-bed river, New Zealand / Geological Society, London, Special Publications, 75:241-255, doi:10.1144/GSL.SP.1993.075.01.15 --- Colin R. Thorne, Andrew P. G. Russell, and Muhammad K. Alam: Planform pattern and channel evolution of the Brahmaputra River, Bangladesh / Geological Society, London, Special Publications, 75:257-276, doi:10.1144/GSL.SP.1993.075.01.16 --- C. S. Bristow: Sedimentary structures exposed in bar tops in the Brahmaputra River, Bangladesh / Geological Society, London, Special Publications, 75:277-289, doi:10.1144/GSL.SP.1993.075.01.17 --- C. S. Bristow: Sedimentology of the Rough Rock: a Carboniferous braided river sheet sandstone in northern England / Geological Society, London, Special Publications, 75:291-304, doi:10.1144/GSL.SP.1993.075.01.18 --- Andrew D. Miall: The architecture of fluvial-deltaic sequences in the Upper Mesaverde Group (Upper Cretaceous), Book Cliffs, Utah / Geological Society, London, Special Publications, 75:305-332, doi:10.1144/GSL.SP.1993.075.01.19 --- John H. Martin: A review of braided fluvial hydrocarbon reservoirs: the petroleum engineer’s perspective / Geological Society, London, Special Publications, 75:333-367, doi:10.1144/GSL.SP.1993.075.01.20 --- W. P. Karpeta: Sedimentology and gravel bar morphology in an Archaean braided river sequence: the Witpan Conglomerate Member (Witwatersrand Supergroup) in the Welkom Goldfield, South Africa / Geological Society, London, Special Publications, 75:369-388, doi:10.1144/GSL.SP.1993.075.01.21 --- Lisa Edgington and Neil Harbury: Provenance of braided alluvial deposits of the Thari Formation, Rhodes, SE Aegean: evidence for major erosion of an ophiolite-bearing thrust sheet / Geological Society, London, Special Publications, 75:389-403, doi:10.1144/GSL.SP.1993.075.01.22 --- Victoria R. Copley and John McM. Moore: Debris provenance mapping in braided drainage using remote sensing / Geological Society, London, Special Publications, 75:405-412, doi:10.1144/GSL.SP.1993.075.01.23
    Pages: Online-Ressource (VII, 419 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 0903317931
    Language: English
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  • 2
  • 3
    ISSN: 1420-9098
    Keywords: Formica exsectoides ; nests ; colony cycle ; temperature ; brood ; reproductives
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary The nest structure and colony cycle of a population of Allegheny mound ants,Formica exsectoides, were examined in central Michigan. The dispersion pattern of mounds was random. Nest structure and presence of brood were primarily determined by excavation of twenty-three nests over three intervals from June through September. Additional excavations of five nests in 1990 and ten nests in 1991 provided further details on nest structure and colony cycle. Most galleries occurred within the mound and upper 30 cm of soil, but some activity reached depths of 100 to 270 cm. Depth of nests showed little correlation with external measurements of height and diameter. Immature stages were recovered from two strata: the upper 20 cm of nest and mound and the lowest nest depths. Alate sexual forms were found in or near the mound in July, and numerous dealate queens were collected in September from peripheral galleries near the soil surface.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 196 (1962), S. 364-365 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The hypothesis that the lenticles (or lithophysse) are due to a drawing out by flow of formerly continuous laminae cannot be accepted for two reasons. The first is that the lenticles would show a preferred direction of elongation when viewed in the foliation plane if they were due to a drawing out ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 406 (2000), S. 56-59 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Linear sand dunes—dunes that extend parallel to each other rather than in star-like or crescentic forms—are the most abundant type of desert sand dune. But because their development and their internal structure are poorly understood, they are rarely recognized in the rock ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 39 (1992), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 69 (1980), S. 849-874 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract Following a general review of the Cretaceous and Paleogene geology of Ecuador, we propose a geologic history from early Cretaceous through Oligocene time with emphasis on the coastal part of the country that is based on the interpretive interaction of three oceanic plates (the Bolívar, proto-Nazca, and Nazca) and the continental South American plate. The proposed history invokes large lateral displacements, the intervention of the previously unrecognized Bolívar plate, the development of three successive subduction zones, the formation of a distant oceanic island arc and its subsequent collision with the South American plate, the emplacement of a major olistostrome complex, and an intricate record of displacement on a currently inactive transform fault. The proposed history offers a viable solution to four major problems of the geology of coastal Ecuador.
    Abstract: Résumé Passant en revue la géologie de l'Equateur au Crétacique et Paléogène, les auteurs proposent une histoire géologique allant depuis le Crétacique inférieur à l'Oligocène en mettant l'accent sur la région cÔtière, et en se basant sur l'interaction de trois plaques océaniques (bolivienne, proto-Nasca et Nasca) et de la plaque continentale de l'Amérique du Sud. L'histoire proposée fait appel à de grands déplacements, à l'intervention de la plaque bolivienne non reconnue antérieurement, au développement de trois zones de subduction successives, à la formation d'une guirlande d'Îles océaniques distante et sa collision subséquente avec la plaque de l'Amérique du Sud, à la mise en place d'un grand complexe olistostromique et à un déplacement sur une faille transformante inactive. L'histoire proposée apporte une solution viable à quatre problèmes de la géologie de la Région cÔtière de l'Equateur.
    Notes: Zusammenfassung Aus der Kreide- und Paläogen-Geschichte Ecuadors läßt sich die Entwicklung der Küstenregion ableiten. Sie wird vom Zusammenwirken von drei ozeanischen Platten (Bolivar, Proto-Nazca und Nazca) und der kontinentalen Platte Südamerikas bestimmt. Die Entwicklung umfaßt ausgedehnte Seitenverschiebungen, das Auftreten einer bisher nicht erkannten Bolivar-Platte, die Anlage von drei aufeinanderfolgenden Subduktionszonen, die Bildung eines Inselbogens und die folgende Kollision mit der Südamerikanischen Platte, die Ablagerung eines großen Olisthostrom-Komplexes und die Verschiebungen entlang einer heute inaktiven Transform-Verwerfung. Damit sind eine Reihe von Problemen der Geologie des Küstenabschnittes Ecuadors gelöst.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Oecologia 87 (1991), S. 514-521 
    ISSN: 1432-1939
    Keywords: Ant-aphid association ; Tritrophic interaction ; Oleander ; Argentine ants ; Aphis nerii
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary Oleander aphids, (Aphis nerii), which are sporadically tended by ants, were used as a moded system to examine whether host plant factors associated with feeding site influenced the formation of ant-aphid associations. Seasonal patterns of host plant utilization and association with attendant ants were examined through bi-weekly censuses of the aphid population feeding on thirty ornamental oleander plands (Nerium oleander) in northern California in 1985 and 1986. Colonies occurred on both developing and senescing plant terminals, including leaf tips, floral structures, and pods. Aphids preferentially colonized leaf terminals early in the season, but showed no preference for feeding site during later periods. Argentine ants (Iridomyrmex humilis) occasionally tended aphid colonies. Colonies on floral tips were three to four times more likely to attract ants than colonies on leaf tips, even though the latter frequently contained more aphids. Ants showed a positive recruitment response to colonies on floral tips, with a significant correlation between colony size and number of ants. There was no recruitment response to colonies on leaf tips. These patterns were reproducible over two years despite large fluctuations in both aphid population density and ant activity. In a laboratory bioassay of aphid palatability, the generalist predator,Hippodamia convergens, took significantly more aphids reared on floral tips compared to those reared on leaf tips. The patterns reported here support the hypothesis that tritrophic factors may be important in modifying higher level arthropod mutualisms.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Medical & biological engineering & computing 22 (1984), S. 55-62 
    ISSN: 1741-0444
    Keywords: Cerebral blood flow ; Impedance plethysmography ; Intraventricular haemorrhage ; Microcomputer ; Neonates ; Signal processing
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Medicine
    Notes: Abstract Electrical impedance measurements can provide much useful information on cerebral haemodynamics in ill newborn infants. However, the analysis of the pusatile impedance signal presents a number of problems. These are due to the electrical noise generated by other monitoring equipment in the neonatal intensive care unit, the presence of a strong breathing component within the impedance signal and frequent movement artefacts. Algorithms based on techniques such as digital filtering, coherent averaging and template matching have been developed to deal with these problems. The continuous analysis of the pulsatile impedance waveforms to be carried out automatically.
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2021-11-09
    Description: The shallow subsurface structure of the 2009 April 6 Mw 6.3 L’Aquila earthquake surface rupture at Paganica has been investigated with ground penetrating radar to study how the surface rupture relates spatially to previous surface displacements during the Holocene and Pleistocene. The discontinuous surface rupture stepped between en-echelon/parallel faults within the overall fault zone that show clear Holocene/Pleistocene offsets in the top 10 m of the subsurface. Some portions of the fault zone that show clear Holocene offsets were not ruptured in 2009, having been bypassed as the rupture stepped across a relay zone onto a fault across strike. The slip vectors, defined by opening directions across surface cracks, indicate dip-slip normal movement, whose azimuth remained constant between 210◦ and 228◦ across the zone where the rupture stepped between faults. We interpret maximum vertical offsets of the base of the Holocene summed across strike to be 4.5 m, which if averaged over 15 kyr, gives a maximum throw-rate of 0.23–0.30 mm yr–1, consistent with throw-rates implied by vertical offsets of a layer whose age we assume to be ∼33 ka. This compares with published values of 0.4 mm yr–1 for a minimum slip rate implied by offsets of Middle Pleistocene tephras, and 0.24 mm yr–1 since 24.8 kyr from palaeoseismology. The Paganica Fault, although clearly an important active structure, is not slipping fast enough to accommodate all of the 3–5 mm yr–1 of extension across this sector of the Apennines; other neighbouring range-bounding active normal faults also have a role to play in the seismic hazard.
    Description: Published
    Description: 774–790
    Description: 3.2. Tettonica attiva
    Description: JCR Journal
    Description: open
    Keywords: Ground penetration radar ; Aquila earthquake ; extension ; active tectonics ; 04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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