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  • 1
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    In:  J. Geophys. Res., Kunming, China, D. Reidel Publishing Company, vol. 100, no. 2, pp. 20159-20174, pp. L09303, (ISSN: 1340-4202)
    Publication Date: 1995
    Keywords: Review article ; Seismicity ; Fault zone ; JGR
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  • 2
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    In:  Nature, Kunming, China, D. Reidel Publishing Company, vol. 291, no. 2, pp. 645-648, pp. L09303, (ISSN: 1340-4202)
    Publication Date: 1981
    Keywords: Tectonics ; rifting
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  • 3
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    In:  Can. J. Earth Sci., Kunming, China, D. Reidel Publishing Company, vol. 22, no. 2, pp. 108-125, pp. L09303, (ISSN: 1340-4202)
    Publication Date: 1985
    Keywords: Tectonics ; Review article ; basin
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  • 4
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    In:  J. Struct. Geol., Kunming, China, D. Reidel Publishing Company, vol. 4, no. 2, pp. 105-115, pp. L09303, (ISSN: 1340-4202)
    Publication Date: 1982
    Keywords: Geol. aspects ; rifting ; Review article ; Tectonics ; Structural geology ; JSG
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  • 5
    Publication Date: 1998-04-08
    Description: Global Positioning System (GPS) surveys from 1991 to 1997 near Yucca Mountain, Nevada, indicate west-northwest crustal elongation at a rate of 1.7 +/- 0.3 millimeters per year (1final sigma) over 34 kilometers, or 50 +/- 9 nanostrain per year. Global Positioning System and trilateration surveys from 1983 to 1997 on a 14-kilometer baseline across the proposed repository site for high-level radioactive waste indicate that the crust extended by 0.7 to 0.9 +/- 0.2 millimeter per year (50 to 64 +/- 14 nanostrain per year), depending on the coseismic effect of the Ms 5.4 1992 Little Skull Mountain earthquake. These strain rates are at least an order of magnitude higher than would be predicted from the Quaternary volcanic and tectonic history of the area.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Wernicke -- Davis -- Bennett -- Elosegui -- Abolins -- Brady -- House -- Niemi -- Snow -- New York, N.Y. -- Science. 1998 Mar 27;279(5359):2096-100.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉B. Wernicke, M. J. Abolins, R. J. Brady, M. A. House, N. A. Niemi, J. K. Snow, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. J. L. Davis, R. A. Bennett, P. Elosegui, Harvard-Smithsonian Cen.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/9516108" 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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  • 6
    Publication Date: 1993-04-09
    Description: The Landers earthquake, which had a moment magnitude (M(w)) of 7.3, was the largest earthquake to strike the contiguous United States in 40 years. This earthquake resulted from the rupture of five major and many minor right-lateral faults near the southern end of the eastern California shear zone, just north of the San Andreas fault. Its M(w) 6.1 preshock and M(w) 6.2 aftershock had their own aftershocks and foreshocks. Surficial geological observations are consistent with local and far-field seismologic observations of the earthquake. Large surficial offsets (as great as 6 meters) and a relatively short rupture length (85 kilometers) are consistent with seismological calculations of a high stress drop (200 bars), which is in turn consistent with an apparently long recurrence interval for these faults.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Sieh, K -- Jones, L -- Hauksson, E -- Hudnut, K -- Eberhart-Phillips, D -- Heaton, T -- Hough, S -- Hutton, K -- Kanamori, H -- Lilje, A -- Lindvall, S -- McGill, S F -- Mori, J -- Rubin, C -- Spotila, J A -- Stock, J -- Thio, H K -- Treiman, J -- Wernicke, B -- Zachariasen, J -- New York, N.Y. -- Science. 1993 Apr 9;260(5105):171-6.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17807175" 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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  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 441 (2006), S. 1131-1134 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Transient tectonic deformation has long been noted within ∼100 km of plate boundary fault zones and within active volcanic regions, but it is unknown whether transient motions also occur at larger scales within plates. Relatively localized transients are known to occur as both ...
    Type of Medium: Electronic Resource
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  • 8
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    In:  Geological Society Special Publication 321: 1-8.
    Publication Date: 2009-10-15
    Description: After the discovery of thrust-and-nappe structure near the turn of the twentieth century, mountain belts were viewed as a direct expression of horizontal shortening of the continental crust, and continental rifting was viewed as a phenomenon distinct from it. By mid-century, broad consensus had emerged, mainly on the basis of physical reasoning, that thrust-and-nappe structure instead reflected gravity sliding secondary to vertical motions of the crust, as embodied in the influential stockwerk folding hypothesis. In a noteworthy period from 1977 to 1982, informally referred to here as the detachment era', not only did the last vestiges of support for the stockwerk hypothesis evaporate, but large-magnitude extension was discovered throughout the Cordillera, manifest primarily by extensional detachments and metamorphic core complexes. Soon afterward extensional detachments were recognized as a global phenomenon, forcing first-order reinterpretation of field relations in most orogens. Although plate tectonics is indisputably the most profound discovery in Earth sciences in the twentieth century, the detachment era arguably had commensurate impact on field-based interpretations of continental tectonics. Three decades later, controversy persists over the origin of metamorphic tectonites in core complexes, and over the existence and mechanics of slip on shallowly dipping extensional detachments.
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  • 9
    Publication Date: 2013-01-03
    Print ISSN: 0016-7606
    Electronic ISSN: 1943-2674
    Topics: Geosciences
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  • 10
    Publication Date: 2017-01-29
    Description: Compilation and synthesis of neotectonic data from the Great Basin region (western U.S.), based on 173 published studies for 171 faults across the region, offer an unprecedented view into the spatiotemporal evolution of strain release in continental domains, at time scales of 1 k.y. to 1 m.y. The results indicate a mean vertical surface displacement for normal faulting earthquakes of 2 m (approximately two-thirds of events in the 1–3 m range). The distribution of earthquake recurrence intervals is more scattered, with a mode of 1–3 k.y., a mean of 11 k.y., and 15% of recurrence intervals 〉20 k.y. While strike-slip faults nearest the plate boundary show relatively steady slip rates through time, northern Great Basin normal faults have had marked temporal slip-rate variations in the Quaternary. Since 15 ka, strain release has been concentrated near the margins (fault slip rates to 1–2 mm/yr), with the central region being nearly inactive. However, over the past 150 k.y., finite deformation is more evenly distributed as faults show more uniform slip rates (0.2–0.3 mm/yr) consistent with their long-term rates. The paleo-earthquake distribution since ca. 60 ka shows two kinematic patterns: local clusters (episodes of events repeated on a single fault) and regionally distributed faulting (episodes of events distributed across several parallel faults, each with a single event). We thus propose a model for northern Great Basin normal faults where they alternate between (1) transient fast periods (1–2 mm/yr) lasting ~50 k.y., characterized by local clusters; and (2) transient slow periods (0.05–0.1 mm/yr) lasting 200–400 k.y., characterized by regional distributed faulting.
    Electronic ISSN: 1553-040X
    Topics: Geosciences
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