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  • Other Sources  (188)
  • Bornträger  (142)
  • Springer  (21)
  • Cambridge University Press  (10)
  • AGU (American Geophysical Union)  (7)
  • Cushman Foundation for Foraminiferal Research  (7)
  • AGU
  • AGU (American Geological Union)
  • American Meteorological Society
  • Oxford Univ. Press
  • Springer Nature
  • 1970-1974  (184)
  • 1955-1959  (4)
Collection
Source
Keywords
Publisher
Years
Year
  • 1
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    Condensed Matter; Magnetic Properties. Magnetic and Other Properties of Oxides and Related Compounds (1970)
    Springer
    In:  Berlin, Springer, vol. III/4, Part a, no. XVI:, pp. 1-14, (ISBN 0-87590-299-5 (soft cover))
    Details
    Publication Date: 1970
    Keywords: Handbook of geophysics ; Handbook of physics ; Handbook of mineralogy
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Transmission of Information by Orthogonal Functions (1972)
    Springer
    In:  New York, Springer, vol. 113, no. XVI:, pp. 1-14, (ISBN 1-56670-263-3)
    Details
    Publication Date: 1972
    Keywords: Transformations ; squ ; Textbook of informatics ; Textbook of mathematics
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Condensed Matter; Magnetic Properties. Magnetic and Other Properties of Oxides and Related Compounds (1970)
    Springer
    In:  Berlin, Springer, vol. III/4, Part b, no. XVI:, pp. 1-14, (ISBN 0-87590-299-5 (soft cover))
    Details
    Publication Date: 1970
    Keywords: Handbook of geophysics ; Handbook of physics ; Handbook of mineralogy
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Model Seismology, Vol. 2, Data Processing and Interpretation (1971)
    Cambridge University Press
    In:  Cambridge, Cambridge University Press, vol. IUGG Volume 18, no. 85, pp. 175, (3-7723-6434-9)
    Details
    Publication Date: 1971
    Keywords: Seismics (controlled source seismology) ; Textbook of geophysics ; SEModelling ; Data analysis / ~ processing
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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    Messung elastischer Eigenschaften von Gesteinen (1956)
    Springer
    In:  Handbuch der Physik, Berlin, Springer, vol. 17, no. 16, pp. 169-201, (ISBN 0080419208)
    Details
    Publication Date: 1956
    Keywords: Laboratory measurements ; Physical properties of rocks ; Velocity ; Seismics (controlled source seismology) ; cylindrical ; waves ; Mueller ; Muller ; Fluegge ; Flugge
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    BIBLIOGRAPHY SEISMOLOGY
  • 6
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    Internally heated pressure vessels (1971)
    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)
    Details
    Publication Date: 1971
    Keywords: Textbook of physics ; Laboratory measurements ; Stress ; ERYBACKI
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    BIBLIOGRAPHY SEISMOLOGY
  • 7
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    Deep-sea carbonates: Pleistocene dissolution cycles (1973)
    Cushman Foundation for Foraminiferal Research
    In:  The Journal of Foraminiferal Research, 3 (4). pp. 187-195.
    Details
    Publication Date: 2020-05-11
    Description: Foraminiferal evidence from the eastern equatorial Pacific and from the North Atlantic indicates that the dissolution of deep-sea carbonates was intensified during interglacials rather than during glacials, in contrast to widespread opinion. Pleistoccne dissolution cycles introduce a systematic bias into the Interpretation of calcareous fossil assemblages near and below the lysocline zone.
    Type: Article , PeerReviewed
    Format: text
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    PAPER (OCEANREP)
  • 8
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    Growth and Development of Spirula Spirula (1970)
    Cambridge University Press
    In:  Journal of the Marine Biological Association of the United Kingdom, 50 (01). pp. 53-64.
    Details
    Publication Date: 2020-07-16
    Description: Spirula spirula has stimulated considerable interest since it was first discovered. It is a member of one of the two genera of sepioids to frequent oceanic water (the other being Heteroteuthis); it has a unique spiral shell which acts as a buoyancy mechanism and can withstand considerable pressure (Denton, Gilpin-Brown & Howarth, 1967); and, until the capture by the Danish Oceanographical expeditions it was considered very rare, only 12 specimens having been captured. The Dana expeditions caught 193 individuals from 1909 to 1931 and these were described by Kerr (1931) and Bruun (1943,1955). Most of these were caught in the waters around the Canary Islands of the North Atlantic. Bruun (1943) arranged the specimens according to month and size and claimed that two size groups could be distinguished. The specimens were taken over a wide geographical area, in several years and during the months of February (1 specimen), March (40), April (3), May (8), June (1), August (1) and October (23). His conclusion concerning growth depends entirely upon his decision to split the March sample into two year-groups; those above 1.9 cm in ventral mantle length he put in a separate year-class to those below 1.9 cm in ventral mantle length. This division was arbitrary and, one suspects, based on a belief that a one-year life-span was likely. Clearly the growth of Spirula requires further study based on a larger collection and the present paper is an attempt to fulfil this need.
    Type: Article , PeerReviewed
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  • 9
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    Paleomagnetism of deep-sea cores (1972)
    AGU (American Geophysical Union)
    In:  Reviews of Geophysics and Space Physics, 10 (1). pp. 213-249.
    Details
    Publication Date: 2017-01-13
    Description: This review is intended to cover the principal developments that have occurred within the last six years in the paleomagnetic study of marine sediments. Recent work utilizing the reflecting-light microscope indicates that detrital high-temperature Fe-Ti oxides are probably responsible for most of the magnetic remanence in marine sediments. These minerals possess a spectrum of coercivities that makes it necessary to use alternating-field—demagnetization techniques to isolate stable components. It is possible to use the standard magnetic stratigraphy for the last 4 m.y. of earth history derived from terrestrial lavas. Using the ages of the magnetic boundaries from this time scale it is possible by extrapolation and interpolation to better determine the ages of the major events. The ages of these events in increasing age are Jaramillo, 0.87 to 0.92 m.y.; Olduvai, 1.71 to 1.86 m.y.; Kaena, 2.82 to 2.90 m.y.; Mammoth, 3.0 to 3.085 m.y.; Cochiti, 3.72 to 3.82 m.y.; Nunivak, 3.97 to 4.14 m.y.; ‘c’ event of the Gilbert series, 4.33 to 4.65 m.y. Through the use of long cores from the central Pacific and through correlation using fossil datums, it has been possible to extend the magnetic stratigraphy back to the upper middle Miocene to magnetic epoch 5. It is concluded that very short magnetic events are probably short-term excursions of the field and not true magnetic events. It is shown that the field of the earth averages to an axial-dipole field within a period of 27,000 years and that the field over the last two million years has acted as a geocentric axial dipole. The evidence shows that when reversals of the dipole occur, the values of the reversed inclination are not significantly different from the normal values. The use of magnetic stratigraphy in marine geology has opened up a new era in study of sedimentary processes and evolution of marine organisms.
    Type: Article , PeerReviewed
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  • 10
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    Temperatures and compositions of magmas ascending along mid-ocean ridges (1973)
    AGU
    In:  Journal of Geophysical Research, 78 (17). pp. 3340-3355.
    Details
    Publication Date: 2020-07-24
    Description: The application of plagioclase geothermometry to plagioclase-bearing volcanic ash layers and to the glassy margins of pillow basalts from the fast-spreading East Pacific rise, the moderately spreading Gorda and Juan de Fuca ridges, and the slow-spreading mid-Atlantic ridge has shown that magma temperatures, as well as average An contents of plagioclases, are negatively correlated with spreading rates. A detailed investigation of the major element chemistry of volcanic glasses from each of these areas suggests that the observed consistent element-element covariances among individual populations of samples have been caused by fractional crystallization of the magmas. The regularity of chemical variation and the similarity of magma temperatures within each population of samples suggest that magmas ascending from beneath each ridge have had similar evolutionary histories. Vector analysis of the chemical data of all samples of volcanic glasses indicate that each population of samples from each of the spreading centers is chemically distinct, even though all samples have been subjected to similar amounts of fractional crystallization. The compositional distinctiveness of each population of oceanic tholeiites probably reflects differences in the depths at which the magmas were generated. Calculated magma temperatures and geothermal gradients calculated from published heat flow measurements can be used to estimate depths of magma generation of about 16 km beneath the East Pacific rise and about 23 km beneath the mid-Atlantic ridge.
    Type: Article , PeerReviewed
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