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  • English  (3,236)
  • Spanish  (25)
  • Arabic  (3)
  • 1995-1999  (2,143)
  • 1960-1964  (1,121)
Collection
Language
Years
Year
  • 1
    Journal available for loan
    Journal available for loan
    Tübingen : Mohr Siebeck ; 1.1884 - 48.1931; N.F. 1.1932/33 - 10.1943/44(1945),3; 11.1948/49(1949) -
    Call number: ZS 22.95039
    Type of Medium: Journal available for loan
    Pages: Online-Ressource
    ISSN: 1614-0974 , 0015-2218 , 0015-2218
    Language: German , English
    Note: N.F. entfällt ab 57.2000. - Volltext auch als Teil einer Datenbank verfügbar , Ersch. ab 2000 in engl. Sprache mit dt. Hauptsacht.
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  • 2
    Monograph available for loan
    Monograph available for loan
    [Edgecumbe, N.Z.] : A. Muller
    Call number: M 15.89146
    Description / Table of Contents: An account of the results of the 2 March 1987 earthquake in the eastern Bay of Plenty and the aftermath's effects on the people and places on the Rangitaiki Plains
    Type of Medium: Monograph available for loan
    Pages: 223 S., , Ill.
    Language: English
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Stuttgart : Schweizerbart Science Publishers ; Volume 1, number 1 (1978)-
    Call number: M 18.91571
    Type of Medium: Monograph available for loan
    Pages: 134 Seiten
    ISSN: 2363-7196
    Series Statement: Global tectonics and metallogeny : special issue Vol. 10/2-4
    Classification:
    Tectonics
    Parallel Title: Erscheint auch als Global tectonics and metallogeny
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Madrid : Secc
    Call number: PIK N 456-17-90913
    Type of Medium: Monograph available for loan
    Pages: 536 Seiten
    Series Statement: Ministerio de Transportes Turismo Y Comunicaciones : Publicación Serie A 114
    Parallel Title: 1,1=6; 2,1=13 von Publicaciones / D / Ministerio del Aire, Subsecretaria de Aviación Civil, Servicio Meteorológico Nacional
    Language: Spanish
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 5
    Monograph available for loan
    Monograph available for loan
    Garmisch-Partenkirchen : Institut für atmosphärische Umweltforschung der Fraunhofer- Gesellschaft
    Call number: MOP 44829 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 25 S. , graph. Darst.
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 6
  • 7
    Publication Date: 2018-11-19
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: Spanish
    Type: report , doc-type:report
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  • 8
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    Oslo : ProSus | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-03-26
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 9
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: report , doc-type:report
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  • 10
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    Cheltenham : Elgar | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-04-30
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 11
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    Aldershot : Ashgate | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 12
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    Leiden : Centre of Environmental Science | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 13
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    Cheltenham : Elgar | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 14
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: contributiontoperiodical , doc-type:contributionToPeriodical
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  • 15
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-11-21
    Description: Statisticians avoid getting involved in data analysis, leaving data users on their own in interpreting the results of their work. This is particularly unfortunate in a new area of applied statistics such as environmental accounting with which few are really familiar. Earlier this year data producers and users explored, in a national seminar, possible policy applications of the results of a "green accounting" project in the Philippines. The main findings of the author's contribution to the seminar, on which the present paper is based, are that environmental accounts: (1) present evidence of sustainable economic performance in the country during the relatively short-time period of 1988–1994; (2) provide information for environmental cost internalization; (3) may guide investment to environmentally sound production processes; (4) help to specify and monitor policies of natural wealth conservation, distribution and management; and (5) reveal major data gaps. The paper concludes that environmental accounts help to assess the sustainability of economic growth in terms of broadly defined capital maintenance. The sustainability of development, however, would have to be measured by alternative or supplementary physical indicators linked to quantifiable standards or targets.
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 16
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    Warsaw : Inst. for Sustainable Development | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 17
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-11-21
    Description: The discussion of sustainable development focused attention on new environmental goals and raised the issue of improving resource productivity. A first step towards sustainability would be to slow-down and reduce the man-induced movements of materials: this is the focus of dematerialization approach which emphasizes what socialist countries used to neglect most – minimizing the use of scarce input factors. This paper applies the dematerialization approach to the discussion on sustainable development in central and eastern Europe. In the early 1990s all countries in eastern Europe have developed new environmental programs which mainly focus on reducing pollution. Environmental strategies focusing on reducing emissions are important but not sufficient for reaching sustainability. A new orientation in the environmental policy in the young market economies is required. Dematerialization approach can be a new option for environmental policy in central and eastern Europe. Dematerialization requires a mix of instruments. Important role can be played by an ecological fiscal reform which covers ecological tax reform and the restructuring of subsidies.
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 18
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    Rohtak : Spellbound | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 19
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    Bonn : Bundesamt für Bauwesen und Raumordnung | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-03-26
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 20
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    Kairo : Friedrich-Ebert-Stiftung | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2017-04-10
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: Arabic
    Type: report , doc-type:report
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  • 21
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    Cologne : TÜV Rheinland Safety and Environmental Protection | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:380
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 22
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    Cheltenham : Elgar | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 23
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 24
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 25
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: contributiontoperiodical , doc-type:contributionToPeriodical
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  • 26
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    Paris : OECD | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:380
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 27
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    Den Haag : Ministerie van Volkshuisvesting, Ruimtelijke Ordening en Milieubeheer | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:380
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 28
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    Den Haag : Ministerie van Volkshuisvesting, Ruimtelijke Ordening en Milieubeheer | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 29
    Publication Date: 2018-11-21
    Description: It is not the scarcity of resources that constitutes environmental problems, but their use, the physical throughput of our economies. Material flows are a proxy for the totality of the unspecific environmental risks from human activities. As a strategic goal, an increase of the life-cycle-wide resource productivity by a factor 10 is suggested, including the materials bought and sold and the not-valued materials: we have to take into account the product itself and its "ecological rucksack". Material flows are best measured at the input side of the economy, where their number as well as the number of entry gates is limited. Thus here regulation and economic incentives can work more efficiently and less bureaucratically than today. The material intensity of products and services can be expressed as MIPS, the material input per unit of service, and as TMR, the total material requirement on the macro level, an important element in physical input–output tables.
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 30
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    Berlin : Federal Ministry for the Environment, Nature Conservation and Nuclear Safety | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 31
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    Leiden : Centre for Environmental Science | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 32
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    Oxford : Oxford Univ. Press | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 33
    Publication Date: 2016-04-28
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 34
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    Bad Neuenahr-Ahrweiler : Europ. Academy for the Study of Consequences of Scientific and Technological Advance | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 35
    Publication Date: 2016-04-28
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 36
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    Den Haag : Ministerie van Volkshuisvesting, Ruimtelijke Ordening en Milieubeheer | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 37
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    Brussels : Europ. Commission | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 38
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 39
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2014-08-15
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 40
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    Heidelberg : Physica-Verl. | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 41
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    Warsaw : Inst. for Sustainable Development | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 42
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    London : Routledge | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2016-04-28
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
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  • 43
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    Washington, DC : American Inst. for Contemporary German Studies | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-11-19
    Keywords: ddc:380
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
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  • 44
    Publication Date: 2018-11-19
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
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  • 45
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    Gelsenkirchen : Inst. Arbeit und Technik | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2018-11-19
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
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  • 46
    Publication Date: 2018-11-19
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 47
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2022-02-18
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 48
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2022-02-18
    Description: Sustainable development is the globally embraced paradigm for integrating environment and development policies. Agreement ends with attempts at operationalizing the elusive notion of sustainability. A contentious debate among "environmentalists" and "environmental economists" has brought about a confusing proliferation of indicators and policy advice on sustainable development. Greening the monetary national accounts could moderate the debate by generating concepts and indicators which translate environmental concerns into the language of widely used economic variables. The implementation of sustainable growth and development requires more. "Eco-nomic" instruments of environmental cost internalization need to be combined with environmental legislation and regulation. Such reconciliation of environmental and economic policies should be supported by a "social compact" between government and civil society. The sustained implementation of sustainable development depends on it.
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
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  • 49
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2022-02-18
    Description: In this paper the results of an analysis of the material intensity of advanced composite materials are presented. The analysis is based on the MIPS-concept of the Wuppertal Institute which allows the calculation of the overall material intensity of products and services. It can be shown that the production of one kg of E-Glass fibers is connected with the consumption of 6.2 kg materials, 95 kg water and 2.1 kg oxygen which is of similar size compared to the inputs required in steel production. Material inputs required to produce one kg of p-aramid are 37 kg of materials and 19.6 kg air. Values for carbon fibers are even higher yielding to 61.1 kg of abiotic materials and 33.1 kg of air. Similarly, the production of epoxy resins is connected with larger material flows than the production of polyester resins. Of core materials, inputs per kg for PVCfoam exceed those in PUR-foam production by a factor of 1.4 in water to 2.3 in abiotic material consumption. However, ecologically decisive are not the inputs per kg but the material input per service unit. Therefore, the material input per service unit computed for the body of a passenger ship and a robot arm are compared with alternative steel and aluminium versions. Both examples show that in the case of significant inputs during the user phase of products, even a more material intensive investment in the production phase can yield significant ecological benefits over the whole life-cycle compared to metal versions. Improvements can easily reach a factor of two albeit significant potential for engine optimizations have still been neglected. Results already include the actual recycling quota of metals whereas for composites only virgin material has been calculated as any form of real recycling does not actually exist but only certain types of downrecycling. Of those treatment options, first material recycling and second the use in blast furnaces would lead to better results in resource productivity than incineration and landfills. The paper finally draws some conclusions about the potential advantages of material substitution in the automotive industry. Due to the rather short real operation time of cars during their user phase - around six months - an investment in advanced composite materials in car production only results in a significant improvement of the overall eco-efficiency of cars if it allows a substantial weight reduction of the overall vehicle.
    Keywords: ddc:600
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
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  • 50
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2022-02-18
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
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  • 51
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    Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie | Wuppertal : Wuppertal Institut für Klima, Umwelt, Energie
    Publication Date: 2022-02-18
    Keywords: ddc:330
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: workingpaper , doc-type:workingPaper
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  • 52
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    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-05-08
    Description: Inhaltsübersicht : Helmut Keupp & Daria Ivanova: Calcareous dinoflagellate cysts from the Late Jurassic and Early Cretaceous of the Western Forebalkan, Bulgaria … 3-31 ; Helmut Keupp & Rolf Kohring: Kalkige Dinoflagellatenzysten aus dem Obermiozän (NN 11 ) W von Rethimnon (Kreta) … 33-53 ; Dimitris Frydas, Helmut Keupp & Spyridon M. Bellas: Biostratigraphical research in Late Neogene marine deposits of the Chania Province, western Crete, Greece … 55-67 ; Glenn Fechner: "Microforaminiferal" lining taphonomy: A cautionary note … 69-81 ; Uwe Gloy & Rolf Kohring: Py-GC-Analysen an einem fossilen Harz aus dem Oberen Jura (Grube Guimarota/Portugal) … 83-88 ; Joachim Gründel: Truncatelloidea (Littorinimorpha, Gastropoda) aus dem Lias und Dogger Deutschlands und Nordpolens … 89-119 ; Helmut Keupp, Martin Röper & Adolf Seilacher: Paläobiologische Aspekte von syn vivo-besiedelten Ammonoideen im Plattenkalk des Ober-Kimmeridgiums von Brunn in Ostbayern … 121-145 ; Nikolaus Malchus: Identification of larval bivalve shells by means of simple statistics … 147-160 ; Carsten Helm, John W.M. Jagt & Manfred Kutscher: Early Campanian ophiuroids from the Hannover area (Lower Saxony, Northern Germany) … 161-173 ; Christian Neumann: New spatangoid echinoids (Echinodermata) from the Upper Cretaceous of Jordan: taxonomy and phylogenetic importance … 175-189 ; Oldrich Fejfar und Daniela C. Kalthoff: Aberrant cricetids (Platacanthomyines, Rodentia, Mammalia) from the Miocene of Eurasia … 191-206 ; Thekla Pfeiffer: Sexualdimorphismus, Ontogenie und innerartliche Variabilität der pleistozänen Cervidenpopulationen von Dama dama geiselana Pfeiffer 1998 und Cervus elaphus L. (Cervidae, Mammalia) aus Neumark-Nord (Sachsen-Anhalt, Deutschland) … 207-313 ; Beiträge zur Baikal-Rift-Forschung : MJ. Kuzmin et al.: Climatic events in Siberia during upper Brunhes according to the Lake Baikal sedimentary record … 315-323 ; S. K. Krivonogov et al.: The prospects of GIS use in investigation of the Baikal area … 325-328 ; Y. Masuda et al.: Perspective Studies of Freshwater Sponges in Lake Baikal … 329-332 ; Oleg A. Timoshkin: Biology of Lake Baikal: „White Spots“ and Progress in Research … 333-348 ; Bibliographie : Uwe Gloy: Bibliographie 1997, Institut für Paläontologie, FU Berlin … 349-352 ;
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Paläobiologie ; Paläontologie
    Language: German , English
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  • 53
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    International Association of Meteorology and Atmospheric Sciences (IAMAS)
    In:  IAMAS Annual Report
    Publication Date: 2020-02-12
    Language: English
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  • 54
    Publication Date: 2020-02-12
    Description: The PISCO’94 (Proyecto de Investigatión Sismólogica de la Cordillera Occidental, 1994) seismological network of 31 digital broad band and short-period three-component seismometers was deployed in northern Chile between the Coastal Cordillera and the Western Cordillera. More than 5300 local seismic events were observed in a 100 day period. A subset of high-quality P and S arrival time data was used to invert simultaneously for hypocenters and velocity structure. Additional data from two other networks in the region could be included. The velocity models show a number of prominent anomalies, outlining an extremely thickened crust (about 70 km) beneath the forearc region, an anomalous crustal structure beneath the recent magmatic arc (Western Cordillera) characterized by very low velocities, and a high-velocity slab. A region of an increased Vp /Vs ratio has been found directly above the Wadati-Benioff zone, which might be caused by hydration processes. A zone of lower than average velocities and a high Vp /Vs ratio might correspond to the asthenospheric wedge. The upper edge of the Wadati-Benioff zone is sharply defined by intermediate depth hypocenters, while evidence for a double seismic zone can hardly be seen. Crustal events between the Precordillera and the Western Cordillera have been observed for the first time and are mainly located in the vicinity of the Salar de Atacama down to depths of about 40 km.
    Language: English
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  • 55
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    International Association of Geodesy (IAG) Office at Deutsches Geodätisches Forschungsinstitut
    In:  IAG Traveux
    Publication Date: 2020-02-12
    Language: English
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  • 56
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    IUGG Secretariat, CIRES Cooperative Institute for Research in Environmental Sciences
    Publication Date: 2020-02-12
    Language: English
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  • 57
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    In:  Mitteilungen / Deutsche Geophysikalische Gesellschaft
    Publication Date: 2020-02-12
    Language: English
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  • 58
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    In:  Geophysical Journal International
    Publication Date: 2020-02-12
    Description: A 2-D profile for the shear wave velocity and anisotropy between Egypt and Spitsbergen is presented. The profile is constructed using fundamental- and higher-mode Love and Rayleigh waves recorded by stations of the NARS-DEEP, IRIS and GEOFON networks. The surface wave data have been inverted for shear velocity and anisotropy using a waveform inversion. In the eastern Mediterranean lithosphere we observe a large difference (7 per cent) between SH and SV velocities. We interpret this anomaly as an anisotropic oceanic lithosphere beneath the eastern Mediterranean, an interpretation which is consistent with tectonic reconstructions of the region. The east European continent is imaged as a high-velocity body whose thickness increases with the estimated age of the lithosphere. The continental root of the Ukrainian and Baltic shields and east European platform extends to a depth of 200 km. This is in contrast to the surrounding younger continental regions which appear to be less than 100 km thick. We further studied the structure of the continental lithosphere by investigating a possible relation between seismic velocities and tectonic age. Both a logarithmic and a square root relation have been fitted to the average seismic velocities in each tectonic region. The data slightly favour a logarithmic relation but a square root relation cannot be excluded.
    Language: English
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  • 59
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    In:  Journal of Structural Chemistry
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Language: English
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  • 60
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Language: English
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  • 61
    Publication Date: 2020-02-12
    Description: Within the BASIN'96 project (Basin Analysis and Seismic Investigation in North Germany 1996) a marine survey gathered seismic data in the southwest BalticSea to study the Caledonian collisional zone between Baltica to the north and Avalonia to the south. Additionally, the airgun pulses have been observed by several land stations. Special attention was paid to record good quality data on Rügen island aiming at linking offshore and land-seismic wide-angle observations. Therefore, a complex geophone array (the ‘Star of Rügen’) was designed to enhance the signal quality. The Star of Rügen data and other onshore observations in NE Germany and on Bornholm, an island in the BalticSea, have been used for P-wave velocity modelling. Important structures of the transition zone from Palaeozoic western Europe to the Precambrian Baltic Shield are imaged in the resulting three-dimensional velocity model. A pronounced basement high north of Rügen island indicates the location of the Caledonian Deformation Front (CDF). Velocities also reflect other prominent features, such as the Rønne Graben, a pull-apart structure of the Tornquist Zone, and the basement outcrops around Bornholm island. In the investigated area the Moho depth varies between 27 and 33 km. A high-velocity layer in the lower crust below the NE German mainland may indicate genetic relations to Baltica. The structural continuity, however, is disturbed by a velocity decrease in an area north of the CDF. Sporadic, but strong reflections from the upper mantle below the CDF seem to be consistent with the reflection seismic data [DEKORP-BASIN Research Group, 1999. Geology 27(1), 55–58].
    Language: English
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  • 62
    Publication Date: 2020-02-12
    Description: During the TOR-1 passive seismic experiment in 1996/97, a maximum of 139 temporary seismograph stations were operating over the Sorgenfrei-Tornquist Zone (STZ) in an area extending from northern Germany through Denmark to central Sweden. One of the objectives was to study horizontal anisotropy directions in the subcrustal lithosphere and asthenosphere across the Trans-European Suture Zone. To achieve this goal,broad-band and intermediate-period (5 s) data of the TOR-1 stations and additional stations of permanent networks (GRSN, GEOFON) were analysed for splitting of SKS and SKKS phases. As a result of the relatively dense station spacing, the method offers good lateral resolution of anisotropy.Preliminary results suggest that the directions of the fast horizontal S wave velocity are affected by the STZ. In central Europe and southern Sweden, far away from the STZ, fast S wave directions are approximately E-W while they turn more northerly closer to the STZ where they are approximately parallel to the trend of the STZ. No significant shear wave splitting was observed north of 57 degr. N and east of 14 degr. E. Small delay times between 0.2 and 0.5 s observed at the northernmost TOR-1 station T40S and T60S may be controlled by anisotropy in a thickened crust. The mantle contribution of horizontal anisotropy within the STZ is probably constrained to an approximately 60-km-thick zone in the depth range between 70 and 300 km. The observations are consistent with a model where azimuthally anisotropy is not governed by present-day mantle flow in the asthenosphere, but rather is frozen into the subcrustal lithosphere during the last episode of tectonic activity.
    Keywords: 550 - Earth sciences
    Language: English
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  • 63
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    International Association of Geomagnetism and Aeronomy (IAGA)
    In:  IAGA Annual Report
    Publication Date: 2020-02-12
    Language: English
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  • 64
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report
    Publication Date: 2020-02-12
    Description: [...] We develop a regularizing solution procedure accounting for recent theoretical stability estimates. The capabilities of the procedure are shown for a single magnetic field component of the spherical harmonic field expansion beginning from the year 1900 by varying the mantle conductivity model and the degree of smoothness in the regularization. As an example, the radial component of a global (5,5) core-mantle boundary field is calculated for two epochs.
    Language: English
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  • 65
    Publication Date: 2020-02-12
    Description: The coupled plate interface of subduction zones—commonly called the seismogenic zone—has been recognized as the origin of fatal earthquakes. A subset of the after-shock series of the great Antofagasta thrust-type event (1995 July 30; Mw = 8.0) has been used to study the extent of the seismogenic zone in northern Chile. To achieve reliable and precise hypocentre locations we applied the concept of the minimum 1-D model, which incorporates iterative simultaneous inversion of velocity and hypocentre parameters. The minimum 1-D model is complemented by station corrections which are influenced by near-surface velocity heterogeneity and by the individual station elevations. By relocating mine blasts, which were not included in the inversion, we obtain absolute location errors of 1 km in epicentre and 2 km in focal depth. A study of the resolution parameters ALE and DSPR documents the importance of offshore stations on location accuracy for offshore events. Based on precisely determined hypo-centres we calculate a depth of 46 km for the lower limit of the seismogenic zone, which is in good agreement with previous studies for this area. For the upper limit we found a depth of 20 km. Our results of an aseismic zone between the upper limit of the seismogenic zone and the surface correlates with a detachment zone proposed by other studies; the results are also in agreement with thermal studies for the Antofagasta forearc region.
    Language: English
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  • 66
    Publication Date: 2020-02-12
    Description: In December of 1994 a fluid injection experiment which triggered several hundreds of microearthquakes was conducted at the KTB main borehole (Oberpfalz, Germany). These events were recorded with a temporal seismic network at the surface. Out of the complete data set, a cluster of five events recorded at four mini-arrays consisting of eight or nine stations was used to investigate the crustal scattering properties in the vicinity of the KTB. For this purpose, the ‘Double Beam Method’ (DBM; Krüger et al. 1993, 1995, 1996) and the ‘Double Beam Imaging Method’ (Scherbaum, Krüger & Weber 1997) were extended to curved wave fronts to drop the restriction of plane-wave propagation. This technique is used for imaging the crustal scattering strength using earthquake clusters recorded at close-by mini-arrays. The results of the array analysis show that the composition of the P coda is mainly affected by the site location of the arrays. Near-surface and deeper crustal scattering contribute in a very complicated pattern. Furthermore, with the present data set it was possible to identify reflections from the top of the Erbendorf Body. This is a very pronounced arrival in most of the recorded traces. In one of the arrays its amplitudes are even greater than the direct P phases. Five to eight coherent phases could be identified by the mini-arrays. Using only these phases, synthetic P-coda traces were constructed, which only contain the coherent part of the observed wavefield. By subtracting the synthetic coherent wavefield from the original traces we achieve a variance reduction in the P coda of up to 37 per cent. This leads to the conclusion that a large amount of the P coda at the KTB can be modelled by a simple deterministic single-scattering model using a small number of individual scatterers.
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  • 67
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    In:  Geophysical Journal International
    Publication Date: 2020-02-12
    Description: High noise levels hamper teleseismic shear wave splitting measurements, which bandpass filtering does not always help. To investigate how robust splitting measurements are to noise, we analysed a set of synthetic records with known splitting parameters and added fixed levels of noise. In the presence of weak anisotropy, single-waveform splitting measurements are unreliable when operating with noisy data sets. A practical rule in terms of S/N ratio and splitting delay time parameters is that splitting is confidently detectable at S/N 〉 8, regardless of the wave's original polarization orientation. However, for the evidence of weak anisotropy to be detectable and measurable at an S/N value of 4, the backazimuth separation of the phases from the fast polarization direction needs to be higher than 20°. Stacks of individual measurements consistently yield reliable results down to S/N values of 4. Applying stacking to data from DSB (Dublin, Ireland), the fast polarization direction φ and lag time δt are 58° and 0.95 s. This orientation reflects surface trends of deformation in the area, as found elsewhere in the UK. Our result thus reinforces the proposed model that the detected anisotropy in the British Isles originates from lithospheric coherent deformation preserved from the last main tectonic episode.
    Language: English
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  • 68
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    In:  IAG National Reports
    Publication Date: 2020-02-12
    Language: English
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  • 69
    Publication Date: 2020-02-12
    Description: This paper presents the application of the electrical resistivity tomography (ERT) method to the investigation of the Tertiary maar structure of Baruth (Germany) known from previous gravimetric surveys. ERT was applied to support the optimum location for a palaeoclimatological drill hole. Special modifications of data acquisition, signal processing and inversion are introduced to adapt the method of ERT to the special requirements for the 3-D investigation of structures with horizontal extensions of 1 km or more. More than 5000 dipole–dipole combinations were recorded at three concentric circular electrode arrangements using stand-alone transient data acquisition systems (RefTek). We present a fast approximate imaging technique based on the simultaneous iterative reconstruction technique (SIRT). As the complete calculation of the inverse Frechét matrix is avoided, the algorithm is especially suitable for large data and model spaces, where complete inversion is beyond the limits of available computing hardware. The single-step method is applicable to arbitrary irregular electrode layouts. Synthetic tests show that the imaging procedure reconstructs the main features of the subsurface. A low-resistivity body could be interpreted as limnic sediments filling the interior of the Tertiary maar crater. Considering the horizontal resistivity gradient, estimates for the lateral and depth extents of the structure were made. An optimum position for a palaeoclimatological borehole was found, and was in good agreement with the gravimetric minimum.
    Language: English
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  • 70
    Publication Date: 2020-02-12
    Description: A marine seismic reflection survey was carried out in 1996 by DEKORP, Potsdam, and BGR, Hannover in the SW Baltic Sea. Several tectonic lineaments were crossed nearly perpendicularly, for example, the Caledonian Deformation Front which is assumed to mark the northern boundary of the terrane Avalonia which accreted to Baltica ca. 400 Ma. Here, a bivergent collision is clearly observed, confirming early ideas from the BABEL survey. The NE-dipping reflections in the uppermost mantle are interpreted as signs of the subducted Tornquist Ocean. A similar tectonic style of compression and indentation is observed in the Proterozoic crust northeast of Bornholm, where in addition a remarkable crustal thickening and a strong increase of reflection power is observed. The three DEKORP lines in this area provide a certain three-dimensional control and allows extension of similar observations from the BABEL line A southward. This Proterozoic terrane accretion seems to be connected to major tectonic lineaments in southern Sweden, either to the Gothian Thrust or the Sveconorwegian Front.
    Language: English
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  • 71
    Publication Date: 2020-02-12
    Description: Oxygen-isotope ratios of precipitation (δ18OP) inferred from deep-lake ostracods from the Ammersee (southern Germany) provide a climate record with decadal resolution. The record in detail shows many of the rapid climate shifts seen in central Greenland ice cores between 15,000 and 5000 years before the present (B.P.). Negative excursions in the estimated δ18OP from both of these records likely reflect short weakenings of the thermohaline circulation caused by episodic discharges of continental freshwater into the North Atlantic. Deviating millennial-scale trends, however, indicate that climate gradients between Europe and Greenland changed systematically, reflecting a gradual rearrangement of North Atlantic circulation during deglaciation.
    Keywords: 550 - Earth sciences
    Language: English
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  • 72
    Publication Date: 2021-08-14
    Description: The history of the study of Polar Motion began with the derivation of the equations for the rotation of a rigid body by Euler published in 1758. This was followed by further theoretical contributions made by Lagrange (1788) and Poinsot (1834). To confirm the existence of the polar motion of the Earth in terms of a variation of latitude, intensive efforts were undertaken at several observatories toward the end of the 19th century. During the 7th General Conference of the European Arc Measurement in Rome in October 1883, Fergola had already suggested to investigate the problem. The latitude variation was detected by K¨ustner at the Berlin Observatory in 1888. Following this, during the Annual Conference of the Permanent Commission of the ”Internationale Erdmessung” in Salzburg in September 1888, Foerster proposed to consider the variation of latitude more systematically by a Special Commission. Activities began quickly, and after considerable effort the International Latitude Service (ILS) started in September 1899. The paper reviews, in which way the Geodetic Institute Potsdam contributed to the foundation of the ILS and took part in its activities through the work of Helmert, Albrecht,Wanach and Mahnkopf. Based on international scientific cooperation, the results were the rectangular coordinates of the Polar Motion from 1890.0 to 1922.7 at 0.1 year intervals, in particular those derived from the latitude observations at independent stations from 1890.0 to 1899.8, and those derived from the latitude observations at the ILS stations from 1899.9 to 1922.7
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  • 73
    Publication Date: 2021-08-14
    Language: English
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  • 74
    Publication Date: 2020-02-12
    Description: The large-scale seismic experiment POLONAISE'97 investigated the seismic structure of the crust and the uppermost mantle in the Polish region of the Trans-European Suture Zone. This paper covers the interpretation of seismic data along the 300-km-long P3 profile, which is located in the Precambrian East European Craton (EEC) parallel to the Teisseyre–Tornquist Zone. The recordings were of high quality, with seismic energy detectable out to 300 km offsets. The crustal model developed by two-dimensional raytracing forward modelling and waveform analysis is characterized by a subhorizontal uniform structure, although the boundaries of several large basement features are crossed. The crystalline crust consists of three parts: the upper, middle and lower crust with P-wave velocities of 6.1–6.4 km/s, 6.55–6.7 km/s and 7.05–7.15 km/s respectively. The PmP wave can usually be correlated at distances beginning at about 100 km, but it has variable reflection character. Moho depth increases from 38 km at the NW end of the profile to 44 km at the SE end. The Pn velocity of 8.05–8.1 km/s is less than that previously found in neighbouring areas of the EEC. The VP/VS ratio was determined separately for the upper/middle and lower crust to be 1.67 and 1.77 respectively. Following the Pn wave, another phase with an apparent velocity of about 8.3 km/s is interpreted as a weak reflection from a low-contrast discontinuity in the uppermost mantle.
    Language: English
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  • 75
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report STR
    Publication Date: 2021-08-21
    Language: English
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  • 76
    Publication Date: 2024-05-02
    Language: English
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  • 77
    Call number: ZSP-387-12
    In: International project on paleolimnology and late cenozoic climate
    Type of Medium: Series available for loan
    Pages: 128 S. : Ill., graph. Darst.
    Language: English
    Branch Library: AWI Library
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  • 78
    Call number: 4/M 98.0541
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: X, 191 S.
    ISBN: 3540650067
    ISSN: 0930-0317
    Series Statement: Lecture notes in earth sciences 80
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 79
    Call number: ZS-190(50) ; ZSP-625-50
    In: PIK report
    Type of Medium: Series available for loan
    Pages: 23 S.
    Series Statement: PIK report 50
    Language: English
    Location: Lower compact magazine
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 80
    Series available for loan
    Series available for loan
    Potsdam
    Associated volumes
    Call number: ZS-190(55) ; ZSP-625-55
    In: PIK report
    Type of Medium: Series available for loan
    Pages: 49 S..
    Series Statement: PIK report 55
    Language: English
    Location: Lower compact magazine
    Location: Lower compact magazine
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  • 81
    Series available for loan
    Series available for loan
    Potsdam
    Associated volumes
    Call number: ZS-190(51) ; ZSP-625-51
    In: PIK report
    Type of Medium: Series available for loan
    Pages: 42 S.
    Series Statement: PIK report 51
    Language: English
    Location: Lower compact magazine
    Location: Lower compact magazine
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  • 82
    Monograph available for loan
    Monograph available for loan
    Rotterdam [u.a.] : Balkema
    Call number: 5/M 03.0165
    Type of Medium: Monograph available for loan
    Pages: 245 S.
    Edition: Revised and updated for the English ed. in 1997-98
    ISBN: 9054107928
    Uniform Title: Mantiinii diapirism
    Classification:
    Geophysics
    Language: English
    Location: Upper compact magazine
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  • 83
    Call number: MOP Per 409/C(269)
    In: Technical memorandum
    Type of Medium: Monograph available for loan
    Pages: 35 S. : Ill., graph. Darst.
    Series Statement: Technical memorandum / European Centre for Medium Range Weather Forecasts 269
    Language: English
    Location: MOP - must be ordered
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  • 84
    Call number: ZS-190(54) ; ZSP-625-54
    In: PIK report
    Type of Medium: Series available for loan
    Pages: 30 S.
    Series Statement: PIK report 54
    Language: English
    Location: Lower compact magazine
    Location: Lower compact magazine
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  • 85
    Series available for loan
    Series available for loan
    Warszawa : Inst. Geofizyki Polskiej Akad. Nauk
    Associated volumes
    Call number: SR 91.0236(D-51) / REgal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 70 S.
    ISBN: 8385173870
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : D, Physics of the atmosphere 51 = 307
    Language: English
    Location: Magazine - must be ordered
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  • 86
    Call number: ZS-190(52) ; ZSP-625-52
    In: PIK report
    Type of Medium: Series available for loan
    Pages: 23 S..
    Series Statement: PIK report 52
    Language: English
    Location: Lower compact magazine
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 87
    Monograph available for loan
    Monograph available for loan
    Dordrecht [u.a.] : Kluwer
    Associated volumes
    Call number: 11/N 01.0383
    In: International tables for crystallography
    Type of Medium: Monograph available for loan
    Pages: xxxi, 992 S.
    Edition: 2nd ed.
    ISBN: 0792352688
    Classification:
    A.3.1.
    Language: English
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  • 88
    Monograph available for loan
    Monograph available for loan
    Hawthorn : Lonely Planet Publ.
    Associated volumes
    Call number: 1.8/M 01.0431
    In: Lonely Planet travel survival kit
    Type of Medium: Monograph available for loan
    Pages: 325 S.
    Edition: 2nd ed.
    ISBN: 0864425562
    Series Statement: Lonely planet
    Classification:
    Geography and Geomorphology
    Language: English
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  • 89
    Call number: M 01.0422
    Type of Medium: Monograph available for loan
    Pages: viii, 325 S.
    ISBN: 0471985732
    Series Statement: British Geomorphological Research Group symposia series
    Classification:
    Sedimentology
    Language: English
    Location: Upper compact magazine
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  • 90
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 4/M 02.0106
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: X, 652 S.
    ISBN: 3540635033
    Series Statement: Lecture notes in earth sciences 83
    Classification:
    Geomagnetism, Geoelectromagnetism
    Language: English
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  • 91
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Associated volumes
    Call number: ZSP-168-300
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 239 S. : Abb. ; 24 cm
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 300
    Language: English
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  • 92
    Call number: AWI G4-00-0135
    In: International hydrology series
    Type of Medium: Monograph available for loan
    Pages: xiv, 140 S. : graph. Darst.
    ISBN: 052163332X
    Series Statement: International hydrology series
    Language: English
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  • 93
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Associated volumes
    Call number: ZSP-168-301
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 229 S. : Abb. ; 24 cm
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 301
    Language: English
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  • 94
    Unknown
    Chichester [u.a.] : Wiley & Sons
    Call number: 94.0579 (VERLUST)
    Pages: xiii, 352 S.
    ISBN: 0471926531
    Classification:
    Photogrammetry, Remote Sensing
    Language: English
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  • 95
    Monograph available for loan
    Monograph available for loan
    London : Imperial College Press
    Call number: AWI A13-00-0113
    Type of Medium: Monograph available for loan
    Pages: XIX, 318 Seiten , illustrationen
    ISBN: 1860941141
    Series Statement: Series on Environmental Science and Management 2
    Language: English
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  • 96
    Call number: AWI A7-99-0178 ; ZSP-287-001
    In: Forschungsberichte
    Type of Medium: Monograph available for loan
    Pages: 20 S.
    Series Statement: Forschungsberichte, Institut für Geophysik und Meteorologie, Universität Köln 1
    Language: English
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  • 97
    Call number: ZSP-168-315
    In: Berichte zur Polarforschung, 315
    Type of Medium: Series available for loan
    Pages: 268 Seiten , Illustrationen
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 315
    Language: English
    Note: Enthaltener Beitrag: Russian-German cooperation SYSTEM LAPTEV SEA 2000: the Lena Delta 1998 expedition / edited by Volker Rachold and Mikhail Grigoryev with contributions of the participants , Enthaltener Beitrag: EURASIAN ICE SHEETS: expedition to the lake Lyadhej-To (Polar Urals) in July-August 1998/ by Wolf-Dieter Hermichen and Frank Wischer , Contents for "Russian-German cooperation SYSTEM LAPTEV SEA 2000: the Lena Delta 1998 expedition" 1 lntroduction 2 Expedition Itinerary 2.1 Selection of working areas 2.2 General logistics and transport 2.3 Time tables of individual working groups 2.3.1 Team 1 (Samoylov) 2.3.2 Team 2 (Dunay) 2.3.3 Team 3 (Bykovsky) 2.3.4 Team 4 (Sagastyr) 2.4 Appendix Table A2-1: List of participants Table A2-2: Participating institutions 3 Modern Processes i n Permafrost Affected Soils 3.1 General lntroduction 3.2 Investigation site ,,Samoylov' 3.3 Soils of Samoylov Island 3.3.1 Soil distribution and classification 3.3.2 Soils of the measurement sites 3.4 Energy and water balance of the active layer 3.4.1 Introduction 3.4.2 Field work and methods 3.4.3 First data 3.4.4 Future work 1999 3. 5 Trace gas fluxes in permafrost affected soils 3.5.1 Methane balance 3.5.1.1 Introduction 3.5.1 .2 Methods and fieldwork 3.5.1.3 Results of the soil survey and geological investigations 3.5.1 .4 First results of the methane gas fluxes 3.5.2 CO2-fluxes in permafrost affected soils 3.5.2.1 Introduction 3.5.2.2 Methods and fieldwork 3.5.2.3 Results 3.6 Biological investigations 3.6.1 Botanical research 3.6.2 Soil zoological research 3.6.2.1 Introduction 3.6.2.2 Field work 3.6.2.3 First results 3.6.3 Ornithological observations 3.6.3.1 Methods 3.6.3.2 Results 3.6.4 Distribution and Abundance of Birds in the Lena Delta 3.6.4.1 Introduction 3.6.4.2 Methods and materials 3.6.4.3 Results and discussion 3.7 Further investigations 3.8 References 3.9 Appendix Table A3-1 : List of samples TP 1 Table A3-2: Precipitation and water samples Table A3-3: List of species of the different measurement sites (Site 1 - 3) Table A3-4: Bird species. Lena Delta, rnid-July - August 1998 Table A3-5: Abundance of birds in the channels (inv.110 km) of the different sites of the Lena Delta List A3-1: Description of the soils along the transects of Sarnoylov Island List A3-2: Preliminary total list of plant species from the Sarnoylov Island 4 Modern Sedimentation and Environmental History of the Lena Delta 4.1 lntroduction 4.2 Modern Sedimentation in the Lena Delta 4.2.1 Recent mechanisms of particle transport in the Lena Delta 4.2.2 In-situ conditions of the water column in August 1998 4.2.3 Seasonal changes of water level in the delta region 4.3 Sedimentation and environmental history of the Lena Delta 4.3.1 Introduction 4.3.2 Samples and methods 4.3.3 Field work and preliminary results Arga Island 4.3.4 Field work and preliminary results at Olenyok channel 4.3.5 Field work and preliminary results at Sardakh channel 4.3.6 Field work and preliminary results at Samoylov Island 4.4 Geological-Geomorphological Studies in the Northern Lena River Delta 4.4.1 Introduction 4.4.2 Methods 4.4.3 Study region 4.4.4 Field work results 4.4.5 Conclusions 4.4.6 Acknowledgments 4.5 References 4.6 Appendix Table A4-1: List of stations for hydrological. sedimentological and geophysical investigations Table A4-2: List of sarnples for sedimentological and geochemical investigation Table A4-3: List of samples for Geological-Geomorphological Studies in the Northern Lena River Delta Table A4-4: List of plant species found in the northern Lena River delta 5 Paleoclimate Signals of Ice-rich Permafrost 5.1 Introduction 5.2 Geologie-geomorphological characteristics of the study area 5.3 Modern geological processes on Bykovsky Peninsula 5.4 Ground ice studies 5.4.1 Study subjects. their characteristics 5.4.2 Methods 5.4.3 Sampling conception 5.4.4 First results 5.5 Cryolithological studies 5.5.1 Methods 5.5.2 First results 5.6 Geochronometric age determination 5.7 Paleontological research On the Bykovsky Peninsula 5.7.1 Methods 5.7.2 Collection of large mammal bones 5.7.3 Collection of screened samples for small fossils 5.8 References 5.9 Appendix Table A5-1: List of water and ice samples collected on Bykovsky Peninsula during field season 1998 Table A5-2: List and description of sediment samples collected on Bykovsky Peninsula Table A5-3: List of bone samples submitted to the Radiocarbon Laboratory of the Geological Institute, Russian Academy of Sciences Table A5-4: List of samples collected for absolute age determinations Table A5-5: List of bone samples Table A5-6: List of screened samples for small fossils from the sediments of the Bykovsky Peninsula
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  • 98
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Blackwell Science
    Call number: AWI G1-99-0258
    Description / Table of Contents: The record of tectonic and climatic processes through geological time is held within sedimentary rocks along with evidence for the evolution of life on Earth. The study of the formation, transport and deposition of material to form sedimentary rocks and the temporal and spatial relationships between strata is a fundamental part of the Earth sciences. Sedimentology and Stratigraphy aims to provide students who are starting to study geology at university level with an introduction to the continuum of scales of observation and interpretation which lie between the formation of a grain of sand and a fill of a sedimentary basin. In the first section of this book, the author treats the formation and transport of sediment in a largely descriptive manner and introduces the concepts of environments and facies. The full spectrum of continental and marine sedimentary environments is then covered in a series of chapters which consider the depositional processes and products which may be considered to be characteristic for each setting. In the final part, the principles of stratigraphy and interpretation of the fill of sedimentary basins are considered. The text and illustrations are designed to be accessible to those completely new to the subject whilst at the same time the book covers the concepts and terminology used in more advanced work.
    Type of Medium: Monograph available for loan
    Pages: X, 355 Seiten , Illustrationen
    Edition: First published
    ISBN: 0632035781
    Language: English
    Note: Contents: Preface. - 1 Introduction: sedimentology and stratigraphy. - 1.1 Sedimentology and stratigraphy in Earth sciences. - 1.2 Stratigraphy and sedimentology. - 1.3 See the world in just one grain of sand. - 1.4 Processes and products. - 1.5 Sedimentary environments and facies. - 1.6 Modem and ancient sedimentary environments. - 1.7 Geographical distribution of environments and facies. - 1. 8 Changing environments and facies through time. - 1.9 The stratigraphic record and geological time. - 1.10 Earth history, global tectonics, climate and evolution. - 2 Terrigenous clastic sediments: gravel, sand and mud. - 2.1 The components of sediments and sedimentary rocks. - 2.2 Classification and nomenclature of terrigenous clastic sediments and sedimentary rocks. - 2.3 Gravel and conglomerate. - 2.4 Sand and sandstone. - 2.5 Clay, silt and mudrock. - 2.6 Description of the textures of terrigenous clastic sedimentary rocks. - 2.7 Granulometric and clast shape analysis. - 2.8 Maturity of terrigenous clastic material. - 2.9 Terrigenous clastic sediments: summary. - Further reading. - 3 Biogenic, chemical and volcanogenic sediments. - 3.1 Limestone. - 3.2 Volcanic and volcaniclastic rocks. - 3.3 Evaporite minerals. - 3.4 Cherts. - 3.5 Phosphates. - 3.6 Sedimentary ironstone. - 3.7 Carbonaceous (organic) deposits. - 3.8 The description of sedimentary rocks in hand specimen. - 3.9 Examination of sedimentary rocks under the microscope. - Further reading. - 4 Processes of transport and sedimentary structures. - 4.1 Transport media. - 4.2 The behaviour of fluids and particles in fluids. - 4.3 Flows, sediment and bedforms. - 4.4 Waves. - 4.5 Sedimentary structures in sand-mud mixtures. - 4.6 Mass flows. - 4.7 Mudcracks. - 4.8 Erosional sedimentary structures. - 4.9 Sedimentary structures and sedimentary environments. - Further reading. - 5 Environments and facies. - 5.1 Interpreting past depositional environments. - 5.2 The concept of 'facies'. - 5.3 Distribution of palaeoenvironments in time and space. - 5.4 Palaeocurrents. - 5.5 Provenance. - 5.6 Graphic sedimentary logs. - 5.7 Facies and environments: summary. - Further reading. - 6 Continents: sources of sediment and environments of deposition. - 6.1 From source of sediment to formation of strata. - 6.2 The formation of mountains and hills. - 6.3 Continental climatic regimes. - 6.4 Surface processes. - 6.5 Weathering processes. - 6.6 Erosion and transport. - 6.7 Factors which influence erosion rates. - 6.8 Continental environments of deposition. - 6.9 Continental environments: summary. - Further reading. - 7 Glaciers and ice caps. - 7.1 Formation of glaciers. - 7.2 Erosion by glaciers. - 7.3 Glacial deposits. - 7.4 Distribution of glacial deposits. - 7.5 Recognition of glacial deposits: summary. - Further reading. - 8 Arid continental depositional environments. - 8.1 Deserts. - 8.2 Wind in deserts. - 8.3 Water in a desert. - 8.4 Alluvial fans. - 8.5 Playa lakes. - 8.6 Life in the desert. - 8.7 Characteristics of the deposits of arid continental environments: summary. - Further reading. - 9 Rivers: the fluvial environment. - 9.1 River forms and patterns. - 9.2 Modern rivers. - 9.3 Floodplains. - 9.4 Ancient fluvial deposits. - 9.5 Palaeocurrents in fluvial systems. - 9.6 Fossils in fluvial environments. - 9.7 Soils and palaeosols. - 9.8 Recognition of fluvial deposits: summary. - Further reading. - 10 Lacustrine environments: fresh and saline lakes. - 10.1 Modern lakes. - 10.2 Morphology and processes in lakes. - 10.3 Lacustrine sediments and facies. - 10.4 Saline lakes. - 10.5 Life in lakes. - 10.6 Lake environments: summary. - Further reading. - 11 The marine realm: morphology and processes. - 11.1 Marine environments. - 11.2 Tides. - 11.3 Wave and storm processes. - 11.4 Thermo-haline currents. - 11.5 Divisions of the marine realm. - 11.6 Chemical and biochemical sedimentation in oceans. - 11.7 Ecology of the seas. - 11.8 Marine environments: summary. - Further reading. - 12 Deltas and estuaries. - 12.1 Deltas. - 12.2 Controls on deltas. - 12.3 Coarse-grained deltas. - 12.4 Delta 'cycles'. - 12.5 Post- and syndepositional effects on deltas. - 12.6 Recognition of deltaic deposits: summary. - 12.7 Estuaries. - 12.8 Recognition of estuarine deposits: summary. - Further reading. - 13 Coastlines: beaches, barriers and lagoons. - 13.1 Coastal environments. - 13.2 Morphological features of coastlines. - 13.3 Clastic coastlines. - 13.4 Carbonate coastlines. - 13.5 Arid coastlines. - 13.6 Recognition of coastal deposits: summary. - Further reading. - 14 Shallow seas. - 14.1 Sediment supply to shallow seas. - 14.2 Shallow marine clastic environments. - 14.3 Storm-dominated shallow clastic seas. - 14.4 Tide-dominated shallow clastic seas. - 14.5 Shallow marine carbonate environments. - 14.6 Carbonate ramps. - 14.7 Rimmed carbonate shelves. - 14.8 Epeiric, drowned and isolated carbonate platforms. - 14.9 Barred basins and saline giants. - 14.10 Criteria for the recognition of shelf sediments. - Further reading. - 15 Deep marine environments. - 15.1 Modem and ancient oceans. - 15.2 Deep marine mass flows. - 15.3 Submarine fans. - 15.4 Contourites. - 15.5 Pelagic and hemipelagic sedimentation. - 15.6 Other features of deep ocean sediments. - 15.7 Fossils in deep ocean sediments. - 15.8 Ancient deep ocean deposits. - 15.9 Recognition of deep ocean deposits: summary. - Further reading. - 16 Volcanic environments. - 16.1 Volcanic and volcaniclastic rocks. - 16.2 Lavas. - 16.3 Volcaniclastic rocks. - 16.4 Environments of deposition. - 16.5 Recognition of volcanigenic deposits: summary. - 16.6 Volcanic rocks in stratigraphy: flows, dykes and sills. - Further reading. - 17 Sediments into rocks: postdepositional processes. - 17.1 Post-depositional modification of sedimentary layers. - 17.2 Post-depositional physical and chemical processes. - 17.3 Nodules and concretions. - 17.4 Clastic diagenesis. - 17.5 Carbonate diagenesis. - 17.6 Post-depositional changes to evaporites. - 17.7 Diagenesis of volcaniclastic sedirnents. - 17.8 Formation of coal and hydrocarbons. - 17.9 Diagenetic processes: summary. - Further reading. - 18 Stratigraphy: concepts and lithostratigraphy. - 18.1 Stratigraphy and geological time. - 18.2 Chronostratigraphy. - 18.3 Physical stratigraphy. - 18.4 Lithostratigraphy. - 18.5 Lithostratigraphic nomenclature. - 18.6 Lithostratigraphy and environments. - 18.7 Lithostratigraphy and geological maps. - 18.8 Lithostratigraphy and correlation. - Further reading. - 19 Biostratigraphy. - 19.1 Strata and fossils. - 19.2 Fossils in stratigraphy. - 19.3 Taxa used in biostratigraphy. - 19.4 Correlating different environments. - 19.5 Biostratigraphic nomenclature. - 19.6 Biostratigraphy and chronostratigraphy. - Further reading. - 20 Dating and correlation techniques. - 20.1 Radiometric dating. - 20.2 Magnetostratigraphy. - 20.3 Other dating methods. - 20.4 Dating in the Quaternary. - 20.5 Correlation. - Further reading. - 21 Sequence stratigraphy and sea level changes. - 21.1 Introduction. - 21.2 Depositional sequences and systems tracts. - 21.3 Facies patterns in depositional sequences. - 21.4 Sequences in carbonate depositional environments. - 21.5 Subdivision of depositional sequences and systems tracts: parasequences. - 21.6 Sequence stratigraphy and depositional environments. - 21.7 Practical sequence stratigraphy. - 21.8 Causes of sea level fluctuations. - Further reading. - 22 Subsurface stratigraphy. - 22.1 Seismic reflection profiles. - 22.2 Interpreting seismic reflections. - 22.3 Structural features on seismic profiles. - 22.4 Seismic facies. - 22.5 Relating seismic profiles to geological cross-sections. - 22.6 Borehole stratigraphy and sedimentology. - 22.7 Subsurface facies analysis. - 22.8 Use of borehole data. - Further reading. - 23 Sedimentary basins. - 23.1 Tectonics of sedimentary basins. - 23.2 Basins related to crustal extension. - 23.3 Basins related to subduction. - 23.4 Basins related to continen
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  • 99
    Monograph available for loan
    Monograph available for loan
    Tokyo [u.a.] : Terra Scientific [u.a.]
    Call number: AWI G4-02-0059
    Description / Table of Contents: Contents: Preface. - 1 Introduction. - 2 Basic Equation of the Material Transport Process. - 3 Fundamental Equations of Advection. - 4 Tidal Current. - 4.1 Resonance Tide and Tidal Current. - 4.2 Tide and Tidal Current in the Channel. - 4.3 Influence of Earth Rotation. - 4.4 Effect of Bottom Friction. - 4.5 Internal Tide and Tidal Current. - 5 Residual Flow. - 6 Tide-Induced Residual Current. - 7 Density-Driven Current. - 7.1 Water Density. - 7.2 Heat and Salt Budgets. - 7.3 Density-Driven Current Due to River Discharge. - 7.4 Density-Driven Current Due to the Buoyancy Supply from the Open Ocean. - 7.5 Density-Driven Current Due to Buoyancy Input from River and Open Ocean. - 7.6 Density-Driven Current Due to the Topographic Heat Accumulation Effect. - 7.7 Density-Driven Current Due to the Horizontal Distribution of Vertical Diffusivity. - 8 Wind-Driven Current. - 8.1 Wind Stress on the Sea Surface. - 8.2 Ekman Spiral. - 8.3 Langmuir Circulation. - 8.4 Amplification of Diurnal Tidal Current by Land-Sea Breeze. - 8.5 Coastal Upwelling. - 8.6 Horizontal and Vertical Circulations. - 8.7 Shelf Wave. - 9 Diffusion and Dispersion. - 9.1 The Concept of Diffusion. - 9.2 The Concept of Dispersion. - 9.3 Estimating Method of the Magnitude of Dispersion Coefficient. - 9.4 Methods to Estimate the Horizontal Eddy Diffusivity. - 9.5 Estimating Method of Vertical Eddy Diffusivity. - 9.6 Double Diffusion. - 10 Water Exchange and Residence Time. - 10.1 Water Exchange Ratio Near the Strait. - 10.2 Water Exchange Ratio in the Whole Bay. - 10.3 Average Residence Time. - 10.4 Estimating the Remnant Function in the Field. - 11 Diagnostic Model and The Euler-Lagrange Method. - 11.1 Diagnostic Model. - 11.2 Euler-Lagrange Method. - 12 Ecosystem Model. - 12.1 Formulation. - 12.2 Examples of an Ecosystem Model. - Index.
    Type of Medium: Monograph available for loan
    Pages: V, 162 S. : Ill., graph. Darst., Kt.
    ISBN: 0792358953
    Series Statement: Ocean sciences research [1]
    Uniform Title: Engan kaiy¯ogaku
    Language: English
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  • 100
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : Cambridge Univ. Press
    Associated volumes
    Call number: PIK N 454-01-0304
    In: International hydrology series
    Type of Medium: Monograph available for loan
    Pages: 140 p.
    Edition: 1. ed.
    ISBN: 052163332x
    Series Statement: International hydrology series
    Language: English
    Location: A 18 - must be ordered
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