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  • Other Sources  (10)
  • 2000-2004  (3)
  • 1970-1974  (7)
  • 1
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    Seismic moment and long-period radiation of underground nuclear explosions (1973)
    In:  Bull. Seism. Soc. Am., Warszawa, American Geophysical Union, vol. 63, no. 1+2, pp. 847-857, pp. L08304, (ISSN: 1340-4202)
    Details
    Publication Date: 1973
    Keywords: Nuclear explosion ; seismic Moment ; Radiation pattern ; Waves ; Seismology ; Muller ; BSSA
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Reflexion seismischer Wellen an der FL-Verwerfung (2002)
    In:  Mittlg. d. dt. Geophys. Ges., Warszawa, American Geophysical Union, vol. 103, no. 2, pp. 13-19, pp. L08304, (ISSN: 1340-4202)
    Details
    Publication Date: 2002
    Keywords: Reflection seismics ; KTB ; Fraenkische ; Linie ; Mueller ; Muller
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Computation of synthetic seismograms with the reflectivity method and comparison with observations (1971)
    In:  Geophys. J. R. astr. Soc., Klagenfurt, Nuclear Technology Publ., vol. 23, no. 3, pp. 417-433, pp. L21601, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1971
    Keywords: Seismology ; Synthetic seismograms ; Reflectivity method ; Mueller ; Muller ; GJRaS
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Seismic reflections from the crystalline crust below the Continental Deep Drilling Site KTB: Modeling and inference on reflector properties (2002)
    In:  J. Geophys. Res., Kunming, China, 3-4, vol. 107, no. B9, pp. ESE 2-1 to ESE 2-15, pp. 2180, (ISSN: 1340-4202)
    Details
    Publication Date: 2002
    Keywords: Reflection seismics ; scientific drilling ; Germany ; Deep seismic sounding (espec. cont. crust) ; 7205 ; Seismology: ; Continental ; crust ; (1242) ; 7203 ; Seismology: ; Body ; wave ; propagation ; 0935 ; Exploration ; Geophysics: ; Seismic ; methods ; (3025) ; JGR ; Mueller ; Muller
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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    Glassy particles in lunar fines (1970)
    In:  Other Sources
    Details
    Publication Date: 2011-08-16
    Description: Apollo 11 lunar fines glassy particles, investigating morphology, optical properties and chemical composition
    Keywords: SPACE SCIENCES
    Type: ; ADEMIE DES SCIENCES
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    NASA TECHNICAL REPORTS
  • 6
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    Organic inclusions within hydrothermal minerals from S.W. Africa and elsewhere. (1972)
    In:  Other Sources
    Details
    Publication Date: 2019-07-27
    Description: It was observed that quartz crystals from veins within a diabase dike of precambrian age from S.W. Africa contain organic particles which closely resemble, in detailed morphology, coacervates, proteinoid microspheres or fossil and recent microorganisms. The microphotospectrographs in visible and near-ultraviolet light of these minute particles revealed a strong absorption peak at the vicinity of 4000 A, which is indicative of lipids. Hydrothermal mineral from veins from a number of other localities proved to contain the biomorphic organic particles. The theoretical significance of these organic particles is discussed with reference to problems of origin of life.
    Keywords: GEOPHYSICS
    Type: International Meeting on Advances in organic geochemistry 1971; Sept. 7-10, 1971; Hanover; Germany
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    NASA TECHNICAL REPORTS
  • 7
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    Indications of high-temperature processes in organic geochemistry (1970)
    In:  Other Sources
    Details
    Publication Date: 2019-07-13
    Description: Carbonaceous complex use as indicators of geothermal history and high temperature organic geochemistry
    Keywords: CHEMISTRY
    Type: INTERNATIONAL CONFERENCE ON ORGANIC GEOCHEMISTRY; Sep 01, 1966; LONDON
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    NASA TECHNICAL REPORTS
  • 8
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    Chemical origins of cells (1970)
    In:  Other Sources
    Details
    Publication Date: 2019-06-27
    Description: Cells chemical origin, discussing terrestrial fractionation, amino acids, macromolecules, metabolism, etc
    Keywords: BIOSCIENCES
    Type: ; 47 (
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    NASA TECHNICAL REPORTS
  • 9
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    Morphology and petrostatistics of regular particles in Apollo 11 and Apollo 12 fines (1971)
    In:  Other Sources
    Details
    Publication Date: 2019-07-13
    Description: Regular particle morphology and petrostatistics in Apollo 11 and 12 lunar fines and conglomerates, using phase contrast and scanning microscopes
    Keywords: SPACE SCIENCES
    Type: LUNAR SCIENCE CONFERENCE; Jan 11, 1971 - Jan 14, 1971; HOUSTON, TX
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    NASA TECHNICAL REPORTS
  • 10
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    Seismic reflections from the crystalline crust below the Continental Deep Drilling Site KTB-modeling and inference on reflector properties (2002)
    AGU (American Geophysical Union)
    In:  Journal of Geophysical Research: Solid Earth, 107 (B9). p. 2180.
    Details
    Publication Date: 2018-04-25
    Description: The three-dimensional (3-D) reflection-seismic data set ISO-89 3D was recorded near the deep borehole KTB in southeastern Germany. Reflections from the SE1 reflector and from the top of the Erbendorf body (EB) in the upper crystalline crust can be identified in 5–10% of the single-shot sections. The reflectors have been first identified in previous studies of stacked and migrated seismic data. In this paper the velocity and density variations of these two structures are estimated in a new way using true amplitude single-shot (vibroseis) data. The method uses the direct wave Pg as a reference phase and models the amplitude ratios of the SE1 and EB reflections to Pg. Modeling in this paper uses a combination of ray theory and the reflectivity method, and the SE1 and the top of the EB are assumed to be obliquely oriented 1-D structures. Pg modeling shows that a depth-dependent velocity function within the uppermost crystalline basement explains the amplitudes and travel times of this phase with sufficient accuracy. The largest observed amplitude ratios SE1/Pg and EB/Pg are explained by laminated models with strong velocity contrasts and with reflection coefficients of magnitude 0.1–0.2 (SE1) and 0.05–0.15 (EB). The total thickness of the reflecting zones is less than ∼300 m. Pg amplitude modeling requires low Qp factors (〈100) to a depth of ∼1 km, whereas at larger depths, values of several hundred are necessary to keep the SE1 and EB velocity contrasts in realistic ranges. Both reflectors can be interpreted as cataclastic zones. For the SE1 this interpretation agrees with the view that it is a steeply dipping thrust fault which continues the tectonic Franconian Lineament into the upper crust. We assume that the EB is the fractured top of a high-velocity zone at depths below ∼10 km, known from earlier wide-angle measurements. Both reflectors have large weakly reflecting or nonreflecting parts. The SE1 is nonreflecting at the intersection with the KTB borehole.
    Type: Article , PeerReviewed
    Format: text
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    PAPER (OCEANREP)
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