@misc {CaltechAUTHORS_https://authors.library.caltech.edu/id/eprint/51034,
    title ="Short-term earthquake hazard assessment for the San Andreas Fault in southern California",
    author = "Jones, Lucile M. and Sieh, Kerry",
    
    
    number = "91-32",
    
    month = "January",
    year = "1991",
    
    
    
    url = "https://resolver.caltech.edu/CaltechAUTHORS:20141029-154001569",
    note = "© 1991 USGS.",
    revision_no = "13",
    abstract = "The southernmost 200 km of the San Andreas fault in California, from Cajon Pass\nsoutheast to Bombay Beach on the Salton Sea (Figure 1), has not produced a major earthquake\nwithin the historic record. Both geodetic evidence of continuing strain accumulation (Savage et al,\n1986) and the occurrence of recent prehistoric large earthquakes (Sieh, 1986; Sieh and Williams,\n1990), however, lead us to conclude that this fault segment will eventually produce great\nearthquakes that pose one of the greatest hazards to southern California. An estimated 1.0-1.5\nmillion people now live adjacent to the San Andreas fault within the projected zone of severe\nshaking for such an earthquake. A magnitude 7.5 to 8.0 earthquake on this segment would also\ncause widespread damage to San Bernardino, Imperial, Riverside, Orange, and Los Angeles\ncounties, which together have over 12 million inhabitants. For these reasons, the Southern San\nAndreas Fault Working Group was formed in 1989 to recommend how the scientific community\nmight best respond to anomalous geophysical activity along the fault, increase our understanding\nof regional seismotectonics, and offer timely scientific advice to state and local governments.",
}
@misc {CaltechAUTHORS_https://authors.library.caltech.edu/id/eprint/55538,
    title ="Seismicity of Southern California: Earthquakes of ML 3.0 and Greater, 1975 through 1983",
    author = "Hutton, L. K. and Allen, C. R.",
    
    
    number = "4207",
    
    month = "January",
    year = "1985",
    
    
    
    
    url = "https://resolver.caltech.edu/CaltechAUTHORS:20150305-102736725",
    note = "Published 1985 by the Seismological Laboratory, California Institute of Technology, Pasadena, California 91125, with assistance from the Earthquake Research Affiliates.",
    revision_no = "15",
    abstract = "The time period since the last published California Institute of\nTechnology (CIT) earthquake catalog (Hileman 1974; Friedman 1976) has\nseen many changes in data analysis and reporting procedures at the\nSeismological Laboratory. CIT merged its operation with the U.S. Geological Survey (USGS) during this period. Digital recording (Johnson\n1979) was introduced in 1977 and computer systems improved several times\nsince. The seismic network itself expanded from 125 stations in 1975 to\nmore than 200 in early 1983 (Figure 1). The result is an agglomeration\nof data that way take a superhuman effort to sort through.\nMuch use can be made, however, of a timely earthquake catalog which\nis restricted to the larger earthquakes. We therefore present as\ncomplete and reliable a list of events of ML 3.0 and greater as\npossible, comprising 3,650 individual earthquakes.",
}
@article {CaltechAUTHORS_https://authors.library.caltech.edu/id/eprint/74136,
    title ="Active Faulting in Northern Turkey",
    author = "Allen, Clarence R.",
    
    
    number = "1577",
    
    month = "January",
    year = "1969",
    
    
    
    
    url = "https://resolver.caltech.edu/CaltechAUTHORS:20170207-130936360",
    note = "The author's work in Turkey was made possible by the generous cooperation of the Minerals Research and Exploration Institute (Maden Tetkik ve Arama Enstitüsü - - M. T. A.), Dr. S. Alpan, General Director. \nThe field work would have been impossible without the kind help of I. Ketin of Istanbul Technical University and Özcan Aksoy of the M. T. A. In addition to the logistical help obtained through Istanbul Technical University \nand the M. T. A., the work was supported by the G. K. Gilbert Award in Seismic Geology administered through the Carnegie Institution of Washington.",
    revision_no = "14",
    abstract = "The North Anatolian fault zone of Turkey has become widely\npublicized in recent years because of the remarkable series of earthquakes\nthat began along it in 1939 -- most of which have been associated with\ndextral surface displacements that have successively delineated the fault\ntrace from east to west (Ketin and Roesli, 1953; Ambraseys and Zátopek,\n1968). It is not so generally recognized that even prior to 1939 the fault\nzone could easily have been recognized on the basis of abundant and through-going\nfeatures of Quaternary displacements, and that the North Anatolian\nfault is almost completely analogous to the better-known active transcurrent\nfaults of the circum-Pacific region, such as the San Andreas fault of\nCalifornia and the Alpine fault of New Zealand.",
}
@techreport {CaltechAUTHORS_https://authors.library.caltech.edu/id/eprint/46538,
    title ="Local Bulletin of Earthquakes in the Southern California Region 1 January 1963 to 31 December 1966",
    author = "Richter, Charles F. and Nordquist, John M.",
    
    
    
    
    month = "February",
    year = "1967",
    
    
    
    
    url = "https://resolver.caltech.edu/CaltechAUTHORS:20140626-144927682",
    note = "Published with the assistance of the Earthquake Research Affiliates",
    revision_no = "9",
    abstract = "The Local Bulletin of the Pasadena Seismological Laboratory has been issued regularly since the beginning of 1934, and the present Bulletin covers the four-year period from 1 January 1963 to 31 December 1966.",
}