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  • 1
    Publication Date: 2015-02-24
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉McGarr, A -- Bekins, B -- Burkardt, N -- Dewey, J -- Earle, P -- Ellsworth, W -- Ge, S -- Hickman, S -- Holland, A -- Majer, E -- Rubinstein, J -- Sheehan, A -- New York, N.Y. -- Science. 2015 Feb 20;347(6224):830-1. doi: 10.1126/science.aaa0494.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉U.S. Geological Survey (USGS), Earthquake Science Center, Menlo Park, CA 94025, USA. mcgarr@usgs.gov. ; USGS, National Water Quality Assessment Program, Menlo Park, CA 94025, USA. ; USGS, Powell Center, Fort Collins, CO 80526, USA. ; USGS, Geologic Hazards Center, Golden, CO 80225, USA. ; U.S. Geological Survey (USGS), Earthquake Science Center, Menlo Park, CA 94025, USA. ; University of Colorado at Boulder, Boulder, CO 80302, USA. ; Oklahoma Geological Survey, Norman, OK 73069, USA. ; Lawrence Berkeley National Laboratory, Berkeley, CA, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25700505" target="_blank"〉PubMed〈/a〉
    Keywords: Disasters/*prevention & control/*statistics & numerical data ; Earthquakes/*statistics & numerical data ; Proportional Hazards Models ; Safety Management/methods ; United States ; Waste Disposal, Fluid/*methods
    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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  • 2
    Publication Date: 1982-12-17
    Description: Two-color laser ranging measurements during a 15-month period over a geodetic network spanning the San Andreas fault near Palmdale, California, indicate that the crust expands and contracts aseismically in episodes as short as 2 weeks. Shear strain parallel to the fault has accumulated monotonically since November 1980, but at a variable rate. Improvements in measurement precision and temporal resolution over those of previous geodetic studies near Palmdale have resulted in the definition of a time history of crustal deformation that is much more complex than formerly realized.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Langbein, J O -- Linker, M F -- McGarr, A -- Slater, L E -- New York, N.Y. -- Science. 1982 Dec 17;218(4578):1217-9.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17802470" target="_blank"〉PubMed〈/a〉
    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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  • 3
    Publication Date: 1986-04-11
    Description: After the January 1983 earthquake swarm, the last period of notable seismicity, the rapid rate of deformation of the south moat and resurgent dome of the Long Valley caldera diminished. Frequently repeated two-color laser ranging measurements made within a geodetic network in the caldera during the interval June 1983 to November 1984 reveal that, although the deformation accumulated smoothly in time, the rate of extension of many of the baselines decreased by factors of 2 to 3 from mid-1983 to mid-1984. Areal dilatation was the dominant signal during this period, with rates of extension of several baselines reaching as high as 5 parts per million per annum during the summer of 1983. Within the south moat, shear deformation also was apparent. The cumulative deformation can be modeled as the result of injection of material into two points located beneath the resurgent dome in addition to shallow right lateral slip on a vertical fault in the south moat.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Linker, M F -- Langbein, J O -- McGarr, A -- New York, N.Y. -- Science. 1986 Apr 11;232(4747):213-6.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17780806" target="_blank"〉PubMed〈/a〉
    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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