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  • Other Sources  (9)
  • AGU  (7)
  • American Institute of Physics (AIP)
  • Nature Publishing Group
  • Nature Publishing Group (NPG)
  • 2010-2014
  • 1985-1989  (9)
  • 1980-1984
  • 1975-1979
  • 1989  (9)
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  • 2010-2014
  • 1985-1989  (9)
  • 1980-1984
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  • 1
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    AGU
    In:  Washington D. C., AGU, vol. 4, no. 3, pp. 2-203, (ISBN: 3-540-41598-X)
    Publication Date: 1989
    Keywords: Plate tectonics ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Stress ; Vanicek
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  • 2
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    AGU
    In:  Washington D. C., AGU, vol. 3, no. ALEX(01)-FR-77-01, AFTAC Contract F08606-76-C-0025, pp. 329, (ISBN 1-903544-06-8)
    Publication Date: 1989
    Keywords: Textbook of geology ; Volcanology ; Earthquake hazard
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  • 3
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    AGU
    In:  Washington D. C., AGU, vol. 5, no. XVI:, pp. 1-14, (ISBN 0-89871-521-0)
    Publication Date: 1989
    Keywords: Earth model, also for more shallow analyses ! ; Plate tectonics ; Geol. aspects ; Deep seismic sounding (espec. cont. crust)
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  • 4
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    AGU
    In:  Bull., Polar Proj. OP-O3A4, Origin and Evolution of Sedimentary Basins and Their Energy, Washington, D.C., AGU, vol. 48, no. 4, pp. 65-71, (ISBN 0080419208)
    Publication Date: 1989
    Keywords: Geol. aspects ; Modelling ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; 8110 ; Tectonophysics ; Continental ; tectonics ; 8165 ; Structural ; geology ; (crustal ; structure ; and ; mechanics) ; 8194 ; Instruments ; and ; techniques
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  • 5
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    AGU
    In:  Washington D. C., AGU, vol. 8, no. XVI:, pp. 1-14, (ISBN: 0-387-30752-4)
    Publication Date: 1989
    Keywords: Data analysis / ~ processing ; Statistical investigations
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  • 6
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    AGU
    In:  Washington D. C., AGU, vol. 8, no. Publ. No. 12, pp. 9, (3-540-24165-5, XXVI + 228 p.)
    Publication Date: 1989
    Keywords: Earth model, also for more shallow analyses ! ; Plate tectonics
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  • 7
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    AGU
    In:  AGU Spring Meeting, S22A-13, Baltimore, AGU, vol. 11, no. CUED/C/Mats/Tr 51, pp. 1414-1415
    Publication Date: 1989
    Keywords: Seismic networks ; Seismic arrays ; Filter- ; Polarization ; Shear waves
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  • 8
    Publication Date: 2018-03-02
    Description: RECENT advances in 40Ar/39Ar dating1,2 have made it possible to date individual K-feldspar grains from Pleistocene tephra, a capability that greatly improves the reliability and temporal resolving power of the method. Here we apply these new techniques to the dating of a phonolite tephra from the East Eifel volcanic field in West Germany, which is sandwiched between loess and palaeosol (alfisol) deposits, and which was therefore erupted during the transition from a glacial to an interglacial period. Our age estimate for this transition is 215±4 kyr (1 σ), which has important implications for the marine δ18O timescale and for models of global climate change during the Pleistocene. The results show that single-grain dating can detect and compensate for the large quantities of xenocrystic contaminants which are found in many tephra deposits. This technique could be used to date the tephra layers found in marine sediment cores and the results could greatly enhance the reliability of the marine δ18O timescale for more rigorous Fourier analysis testing of the Milankovitch hypothesis.
    Type: Article , PeerReviewed
    Format: text
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  • 9
    Publication Date: 2016-06-16
    Description: ROOTH proposed that the Younger Dryas cold episode, which chilled the North Atlantic region from 11,000 to 10,000 yr BP, was initiated by a diversion of meltwater from the Mississippi drainage to the St Lawrence drainage system. The link between these events is postulated to be a turnoff, during the Younger Dryas cold episode, of the North Atlantic's conveyor-belt circulation system which currently supplies an enormous amount of heat to the atmosphere over the North Atlantic region2. This turnoff is attributed to a reduction in surface-water salinity, and hence also in density, of the waters in the region where North Atlantic Deep Water (NADW) now forms. Here we present oxygen isotope and accelerator radiocarbon measurements on planktonic foraminifera from Orca Basin core EN32-PC4 which reveal a significant reduction in meltwater flow through the Mississippi River to the Gulf of Mexico from about 11,200 to 10,000 radiocarbon years ago. This finding is consistent with the record for Lake Agassiz which indicates that the meltwater from the southwestern margin of the Laurentide Ice Sheet was diverted to the northern Atlantic Ocean through the St Lawrence valley during the interval from ~11,000 to 10,000 years before present (yr BP).
    Type: Article , PeerReviewed
    Format: text
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