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  • 1
    Online Resource
    Online Resource
    SeaCities : Urban Tactics for Sea-Level Rise (2021)
    Singapore :Springer Nature Singapore :
    Details
    Keywords: Human geography. ; Environment. ; Natural disasters. ; Environmental management. ; System theory. ; Human Geography. ; Environmental Sciences. ; Natural Hazards. ; Environmental Management. ; Complex Systems.
    Description / Table of Contents: 1. Introduction -- 2. Inter-national examples of Water Hazards -- 3. Tactics and examples against sea-level rise -- 4. Application of tactics in scenarios -- 5. From risks to opportunities Outcome, outlook.
    Abstract: This book presents and discusses a strategy which includes four approaches to dealing with the risk of sea-level rise and other water hazards. It also offers opportunities for cities to explore urban extensions such as marine estates, aquatic food production systems, new sea related industries, maritime transport developments, new oceanic tourist attractions, and the designation of additional coastal ecological zones. The urban interface between Sea and Cities generates, therefore, both burning issues and valuable opportunities and raises the question of whether it is possible to solve the former by exploiting the latter?
    Type of Medium: Online Resource
    Pages: XVII, 304 p. 157 illus., 121 illus. in color. , online resource.
    Edition: 1st ed. 2021.
    ISBN: 9789811587481
    Series Statement: Cities Research Series,
    URL: https://doi.org/10.1007/978-981-15-8748-1
    DOI: 10.1007/978-981-15-8748-1
    DDC: 304.2
    Language: English
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  • 2
    Monograph available for loan
    Monograph available for loan
    World atlas of natural hazards (2004)
    London : Arnold [u.a.]
    Details Availability
    Call number: 8/A3 41
    Type of Medium: Monograph available for loan
    Pages: VII, 120 S. : zahlr. Ill., graph. Darst., Kt. , 37cm
    Edition: 1st publ. in Great Britain
    ISBN: 0340764058
    Classification:
    B..
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Electronic Resource
    Electronic Resource
    Association scan of 14,500 nonsynonymous SNPs in four diseases identifies autoimmunity variants (2007)
    [s.l.] : Nature Publishing Group
    Nature genetics 39 (2007), S. 1329-1337 
    Details
    ISSN: 1546-1718
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Medicine
    Notes: [Auszug] We have genotyped 14,436 nonsynonymous SNPs (nsSNPs) and 897 major histocompatibility complex (MHC) tag SNPs from 1,000 independent cases of ankylosing spondylitis (AS), autoimmune thyroid disease (AITD), multiple sclerosis (MS) and breast cancer (BC). Comparing these data against a common control ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/ng.2007.17
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  • 4
    Electronic Resource
    Electronic Resource
    Genome-wide association study of 14,000 cases of seven common diseases and 3,000 shared controls (2007)
    [s.l.] : Nature Publishing Group
    Nature 447 (2007), S. 661-678 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] There is increasing evidence that genome-wide association (GWA) studies represent a powerful approach to the identification of genes involved in common human diseases. We describe a joint GWA study (using the Affymetrix GeneChip 500K Mapping Array Set) undertaken in the British population, which ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/nature05911
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  • 5
    Electronic Resource
    Electronic Resource
    Microtubules and Filaments Beneath the Fission Furrow of Stentor coeruleus (1983)
    Oxford, UK : Blackwell Publishing Ltd
    The @journal of eukaryotic microbiology 30 (1983), S. 0 
    Details
    ISSN: 1550-7408
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: . The ultrastructure of the cortex beneath the fission furrow of dividing Stentor coeruleus was examined using scanning and transmission electron microscopy. During division, basal bodies, axonemes, and km fibers beneath the furrow were absorbed near the moving primordial oral apparatus, and a circumferential band of microtubules and filaments was formed at the base of the furrow. The location and orientation of this fibrous band suggest that it may be an important component of the cytokinetic machinery. Treatment with vinblastine sulfate (4 × 10-5 M) disrupted the circumferential microtubules and blocked division, which is consistent with this hypothesis.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1550-7408.1983.tb01038.x
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  • 6
    Electronic Resource
    Electronic Resource
    Proximity Effects. XX. Search for Transannular Reactions in Carbon-substituted Cycloöctane Derivatives1 (1960)
    s.l. : American Chemical Society
    Journal of the American Chemical Society 82 (1960), S. 5439-5445 
    Details
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/ja01505a035
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  • 7
    Electronic Resource
    Electronic Resource
    Proximity Effects. XXVIII. The Solvolysis of 5,5-Diphenylcycloöctyl p-Toluenesulfonate1 (1962)
    s.l. : American Chemical Society
    Journal of the American Chemical Society 84 (1962), S. 4855-4862 
    Details
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/ja00883a044
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  • 8
    Electronic Resource
    Electronic Resource
    Coseismic crustal deformation from microseismicity in the Patras area, western Greece (1995)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 122 (1995), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The Patras area lies in the western part of central Greece. It is an area characterized by high seismicity and complex neotectonics. Several devastating earthquakes have occurred in the region since 600 BC. Contemporary crustal deformation is examined in this area using microearthquake data recorded over a lengthy period, during 1983–84, by the Patras Seismic Network, principally, and to a lesser extent by the Volos Seismic Network.The microseismicity (1.8–3.9 ML) defines a zone deepening to the NE, which justifies a possible extension of the Gulf of Corinth major graben towards the Trikhonis Lake to the NW.Spectra of 108 well-located microearthquakes are estimated, using P-waves obtained by selective windowing designed to include only the P-phase; seismic moments in the range 0.3–45.7 × 1012 Nm are obtained, accompanied by estimates of seismotectonic source parameters including source radii, average stress drop and average coseismic slip.Poor correlation is found between seismic moment and magnitude, and the likely reason is the complex nature of the neotectonic regime existing in the area.Two zones differing in crustal deformation characteristics are observed. The Corinth-Trikhonis zone reveals two sets of characteristic faults. The first set is represented by microearthquakes showing distinctive and relatively higher seismic moments in conjunction with lower stress drops and seismic slips. This set of faults shows greater source radius than the second set, and therefore the faults are longer. The second set is characterized by an almost constant source radius within the range of uncertainty, and a wide range of seismic moments, stress drops and seismic slips. The Rio zone is characterized by low seismic slip, stress drop and fault radii, with the exception of the locality south of the city of Patras, where relatively higher seismic slip, stress drop and fault radius are observed.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1995.tb06840.x
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  • 9
    Electronic Resource
    Electronic Resource
    Seismotectonics and the earthquake frequency–magnitude distribution in the Aegean area (1989)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 98 (1989), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: A study of Aegean seismotectonics and the resulting frequency–magnitude distribution on a broad scale is undertaken, using the tectonic model of Le Pichon & Angelier. This implies a tectonic moment release rate due to the spreading of the Aegean of 17 ± 8 times 1018 N m-1 yr-1 over the past 13 Ma, if stretching is due mainly to a series of normal faults dipping at about 45° in a seismogenic crust 10–20 km deep. The moment-magnitude relation from an instrumental magnitude catalogue is log M0=A+Bm, with A= 10.970 ± 0.294, B= 1.206 in SI units. This is established from 50 events of magnitude Ms〉5.3 whose scalar seismic moments M0 have been evaluated in a homogeneous manner for the region by spectral analysis of surface waves at 30–60 s period. By contrast published body-wave analyses, from waveform modelling at 20 s period and moment tensor analyses seem to produce seismic moments which are lower by a factor of two or so on average. This moment–magnitude relation implies a seismogenic moment release rate due to stretching in the Aegean of 14 times 1018 N m-1 yr-1 during the time period 1918–81 and 17 times 1018 N m-1 yr-1 for the period 1964–81, within a factor of two or so uncertainty. This implies that the energy release in the brittle crust due to Aegean spreading is substantially seismic within the stated accuracy, and is also relatively stationary even when compared with the tectonic moment release rates. A similar comparison using the same tectonic model shows that the subducting slab is sinking beneath the Hellenic arc almost completely aseismically, and that processes such as near vertical slab pull and confined thermal expansion could explain most of the observed seismic energy release by internal deformation of the slab. The frequency–magnitude statistics for the area of active extension has a characteristic earthquake of magnitude 7Ms, corresponding approximately to fault depths of 10–14 km for an aspect ratio of 2 and a strain drop of 10-4. This is close to the observed seismogenic depth (10–20 km) for well-determined earthquakes in the Aegean area.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1989.tb02291.x
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  • 10
    Electronic Resource
    Electronic Resource
    Coseismic crustal deformation on a fault zone defined by microseismicity in the Pavliani area, central Greece (1995)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 123 (1995), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Pavliani is an area of high microseismicity in northern central Greece. There is no evidence in the historical record of large damaging earthquakes in this area since at least 600 BC. We examine contemporary crustal deformation in this area using microearthquake data recorded during 1983–84 by the Volos seismic network, principally, and to a lesser extent by the Patras seismic network.The microseismicity (1–4.6 ML) defines an approximately vertical fault zone trending WSW-ENE, of 55 km length and 25 km depth. the fault-plane solution for the 4.6 ML earthquake shows a strike consistent with the trend of the microseismicity zone, and an extension direction consistent with many large earthquakes in central Greece associated with the extensional greater Aegean. Spectra of the microearthquakes are estimated using P waves obtained by selective windowing designed to exclude other P phases from the coda; seismic moments in the range 1–95 x 1012 N m are obtained, accompanied by estimates of seismotectonic source parameters, including source radii, average stress drop and average coseismic slip. of prime utility is an excellent correlation found between seismic moment and magnitude, and with coseismic slip. This allows heterogeneity in the distribution of individual microearthquake source parameters to be mapped onto the vertical fault-zone plane and the history of coseismic deformation for the whole seismicity observed during 1983–84 to be examined using cumulative slip and moment-release rate. Peaks of high moment-release rate occur in the east and centre of the fault zone. That in the east is dominated by a few large moment-release events; that in the centre by a large number of small events. Both moment-release-rate peaks, despite their different component seismicity, are associated with high cumulative coseismic slip. Only the eastern peak is also associated with high stress drop; it is also shallower, and therefore any surficial interaction is less likely to be attenuated. the surface projection of this peak is within 3 km of a mapped normal fault coincident with an Alpine thrust front delineated by a major scarp of Mesozoic limestone. Surface evidence of recent movement on this normal fault is only slight. Friable fault gouge is seen at a few localities. Displacement could not be determined because the limestone surfaces are deeply weathered and lack kinematic indicators. However, considering the whole fault zone as a cohesive entity, and using a Brune estimate of slip at the current moment-release rate throughout the present extensional tectonic regime, suggests a total vertical displacement of order 175 m, similar to the elevation of the scarp.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1995.tb06659.x
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