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  • Other Sources  (41)
  • Springer  (19)
  • Elsevier  (16)
  • ITGE  (6)
  • American Institute of Physics (AIP)
  • 1970-1974  (41)
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Years
Year
  • 1
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    Elsevier
    In:  Amsterdam, Elsevier, vol. 8, pp. 415, (ISBN 0-471-95596-5)
    Publication Date: 1974
    Keywords: Textbook of geophysics ; Data analysis / ~ processing ; Spectral analysis ; Spectrum ; Seismology ; Seismics (controlled source seismology) ; Bath
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  • 2
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    Springer
    In:  Berlin, Springer, vol. III/4, Part a, no. XVI:, pp. 1-14, (ISBN 0-87590-299-5 (soft cover))
    Publication Date: 1970
    Keywords: Handbook of geophysics ; Handbook of physics ; Handbook of mineralogy
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  • 3
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    Springer
    In:  New York, Springer, vol. 113, no. XVI:, pp. 1-14, (ISBN 1-56670-263-3)
    Publication Date: 1972
    Keywords: Transformations ; squ ; Textbook of informatics ; Textbook of mathematics
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  • 4
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    Springer
    In:  Berlin, Springer, vol. III/4, Part b, no. XVI:, pp. 1-14, (ISBN 0-87590-299-5 (soft cover))
    Publication Date: 1970
    Keywords: Handbook of geophysics ; Handbook of physics ; Handbook of mineralogy
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  • 5
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    Elsevier
    In:  Amsterdam, London, New York, xiv+320 pp., Elsevier, vol. 5, no. 22, pp. 662-664, (ISBN 1-4020-1244-6)
    Publication Date: 1974
    Keywords: Earthquake risk ; Earthquake hazard ; Earthquake engineering, engineering seismology ; Seismicity ; Plate tectonics ; Tectonics ; Seismology
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  • 6
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    Springer
    In:  Bull., Polar Proj. OP-O3A4, Research Techniques for High Pressure and High Temperature, New York, Springer, vol. 20, no. XVI:, pp. 217-250, (ISBN: 3-540-23712-7)
    Publication Date: 1971
    Keywords: Textbook of physics ; Laboratory measurements ; Stress ; ERYBACKI
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  • 7
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    ITGE
    In:  Revista Española de Micropaleontologia, 2 (1). pp. 55-84.
    Publication Date: 2017-01-30
    Description: The examination of forty two samples of Sediment coming from the “Golfe de Gascogne” Continental margin (from 150 to 4.200 metres) has established the proof of a fauna rieh in benthic and planktonic foraminifera. This research enables to set up the value of certain foraminiferal associations and to propose a zoned essay based on three major groups touching successively the infralittoral, epibathyal, mesobathyal and abyssal parts.
    Type: Article , PeerReviewed
    Format: text
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  • 8
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    ITGE
    In:  Revista Española de Micropaleontologia, 3 (1). pp. 35-60.
    Publication Date: 2017-02-08
    Description: Young tests studied in very thin sections with the light-microscope with a magnification x 1000 showed, that the results obtained hy Reiss, Be Hemleben and others cannot be true. A primary membrane with sieve-plates where pores are projected by the animal is the first formed membrane; then a hyaline layer is formed beneath the membrane with a general thickness of 2-5 (1 in the Globigerine species. Hie thickness of this primary lamella is also that of the lamella covering the proloculus and the first initial chambers and their septa which always have simple walls. In this primary lamella the pores are spared out and they are at first closed by the sieveplates which, however, may be dissolved soon but for a rim in the wall of the pores. Then a second layer Starts, now at the outside of the primary membrane, beginning with fine knobs between the pores but soon forming a whole layer of clear calcäreous matter. It is in this stage that also the first spines are formed, strengthened at their bases by a mount of calcareous matter; so these spines end at their bases at the primary membrane. The thickening of the outer lamella may continue; this lamella is formed soon after the building of the primary lamella, Not only by means of the study of the last formed chamber of several species of Globigerines this result was obtained, but also by means of the colouring of the layers in Globigerina rubra. It is shown, moreover, that Sphaeroidinella dehiscens cannot be an advanced stage of Globigerina triloba. In Globorotaliid species the primary lamella, as found by Reiss c.s., mostly is slightly thicker than in Globigerines. In this group young specimens were observed with last formed chambers having only the primary lamella covered by the primary membrane also, whereas specimens were found which have septa only built by this lamella. The second, outer lamella is formed soon after the primary lamella, so that many specimens occur which show two lamellae in the wall of the last formed chamber. The result is thus quite similar to that obtained in the Globigerines: the species around Globorotalia are monolamellar too.
    Type: Article , PeerReviewed
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  • 9
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    Elsevier
    In:  Earth and Planetary Science Letters, 17 (2). pp. 397-407.
    Publication Date: 2017-02-14
    Description: Volcanic ash layers, which represent the products of volcanic activity within the ocean basins, are common in sedimentary cores taken near Cobb Seamount and on the actively spreading Gorda and Juan de Fuca Ridges. Petrographic and chemical analyses of the glass shards from these deposits have revealed that they are unaltered and are as chemically representative of local volcanic events as are the glassy margins of fresh pillow basalts recovered from the same areas. The presence of unhydrated glass shards in samples as old as 3.8 my is in direct conflict with published hydration rates of both terrestrial and submarine volcanic glasses. A study of a sequence of ash layers from Cobb Seamount, which spans in time much of the Seamount's history, indicates that the volcanic products from Cobb Seamount have had alkaline affinities and that its eruptions have been becoming progressively enriched in Al2O3. Recent experimental petrological evidence and the data on the chemical compositions of Cobb Seamount and the adjacent Juan de Fuca Ridge magmas are in agreement with the hypothesis that magmas are being generated at progressively greater depths beneath Cobb Seamount as it migrates away from the Juan de Fuca Ridge.
    Type: Article , PeerReviewed
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  • 10
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    Springer
    In:  Fortschritte der Chemie organischer Naturstoffe, 30 . pp. 151-206.
    Publication Date: 2018-04-11
    Description: Mutterkorn, das Dauermycel des auf Roggenähren wuchernden Fadenpilzes Claviceps purpurea, enthält eine Gruppe hellgelber, schwach saurer, optisch aktiver Farbstoffe. Obwohl die ersten Präparate dieser Farbstoffe schon vor fast 100 Jahren von DRAGENDORFF und Mitarb. (14) isoliert wurden, konnte deren Strukturaufklärung im wesentlichen erst in den letzten Jahren durchgeführt werden. Dies ist darauf zurückzuführen, daß für die Reindarstellung der schwer trennbaren, teilweise diastereomeren Farbstoffe leistungsfähige chromatographische Methoden entwickelt werden mußten (1, 27, 29, 47). Als sich gezeigt hatte, daß diese Farbstoffe eine Naturstoffgruppe aus mehr als 10 Vertretern mit sehr ähnlichen Strukturen bilden, wurde für sie der Sammelname Ergochrome und eine einfache Nomenklatur vorgeschlagen (19, 25, 29).
    Type: Article , PeerReviewed
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