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  • Seismology  (4)
  • JGR  (2)
  • *Trans-Activators  (1)
  • Aleutian Arc  (1)
  • Animals  (1)
  • 1990-1994  (6)
  • 1
    Publication Date: 1992
    Keywords: Proceedings of a conference ; Earthquake precursor: prediction research ; Source ; Seismology
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  • 2
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    In:  Phys. Earth Plan. Int., Washington, D.C., AGU, vol. 61, no. 3, pp. 269-290, pp. 1047, (ISSN: 1340-4202)
    Publication Date: 1990
    Keywords: Seismology ; Source ; Source mechanics ; Subduction zone ; PEPI
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  • 3
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    In:  J. Geophys. Res., Warszawa, AGU, vol. 98, no. 6951, pp. 2017-2037, pp. 2091, (ISSN: 1340-4202)
    Publication Date: 1993
    Keywords: Seismology ; Subduction zone ; Hypocentral depth ; JGR
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  • 4
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    In:  J. Geophys. Res., Warszawa, AGU, vol. 96, no. 6951, pp. 11997-12022, pp. 2091, (ISSN: 1340-4202)
    Publication Date: 1991
    Keywords: Subduction zone ; Seismology ; JGR
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  • 5
    Publication Date: 1993-09-24
    Description: Intraperitoneal injection of epidermal growth factor (EGF) into mice resulted in the appearance in liver nuclei of three tyrosine phosphorylated proteins (84, 91, and 92 kilodaltons) within minutes after administration of EGF. Administration of interferon-gamma (IFN-gamma) resulted in the appearance in liver nuclei of two tyrosine phosphorylated proteins (84 and 91 kilodaltons). The 84- and 91-kilodalton proteins detected after either EGF or IFN-gamma administration were identified as the IFN-gamma activation factors (GAF). Furthermore, gel shift analysis revealed that these GAF proteins, detected after either EGF or IFN-gamma administration, specifically bound to the sis-inducible element of the c-fos promoter. Thus, GAF proteins participate in nuclear signaling in both IFN-gamma and EGF pathways.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Ruff-Jamison, S -- Chen, K -- Cohen, S -- HD-00700/HD/NICHD NIH HHS/ -- New York, N.Y. -- Science. 1993 Sep 24;261(5129):1733-6.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Biochemistry, Vanderbilt University School of Medicine, Nashville, TN 37232.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/8378774" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Base Sequence ; Cell Nucleus/drug effects/*metabolism ; DNA-Binding Proteins/*metabolism ; Epidermal Growth Factor/*pharmacology ; Genes, fos ; Interferon-Stimulated Gene Factor 3 ; Interferon-gamma/*pharmacology ; Liver/drug effects/metabolism ; Mice ; Molecular Sequence Data ; Phosphorylation ; Promoter Regions, Genetic ; STAT1 Transcription Factor ; *Trans-Activators ; Transcription Factors/*metabolism ; Tyrosine/*metabolism
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 142 (1994), S. 3-28 
    ISSN: 1420-9136
    Keywords: Subduction zones ; Aleutian Arc ; tsunamis ; earthquake parameters
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The 9 March 1957 Aleutian earthquake has been estimated as the third largest earthquake this century and has the longest aftershock zone of any earthquake ever recorded—1200 km. However, due to a lack of high-quality seismic data, the actual source parameters for this earthquake have been poorly determined. We have examined all the available waveform data to determine the seismic moment, rupture area, and slip distribution. These data include body, surface and tsunami waves. Using body waves, we have estimated the duration of significant moment release as 4 min. From surface wave analysis, we have determined that significant moment release occurred only in the western half of the aftershock zone and that the best estimate for the seismic moment is 50–100×1020 Nm. Using the tsunami waveforms, we estimated the source area of the 1957 tsunami by backward propagation. The tsunami source area is smaller than the aftershock zone and is about 850 km long. This does not include the Unalaska Island area in the eastern end of the aftershock zone, making this area a possible seismic gap and a possible site of a future large or great earthquake. We also inverted the tsunami waveforms for the slip distribution. Slip on the 1957 rupture zone was highest in the western half near the epicenter. Little slip occurred in the eastern half. The moment is estimated as 88×1020 Nm, orM w =8.6, making it the seventh largest earthquake during the period 1900 to 1993. We also compare the 1957 earthquake to the 1986 Andreanof Islands earthquake, which occurred within a segment of the 1957 rupture area. The 1986 earthquake represents a rerupturing of the major 1957 asperity.
    Type of Medium: Electronic Resource
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