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  • 1
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    Surface faulting accompanying the Borah Peak earthquake, central Idaho (1984)
    In:  Geology, Roma, Acad. Roy. des Sciences, vol. 12, no. 33, pp. 664-667, pp. B04102, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1984
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Earthquake ; USA ; Geol. aspects
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Paleoseismology as a tool for understanding Quaternary fault behavior and evaluating seismic hazards in continental regions (1996)
    Inst. f. Theoret. Geodäsie
    In:  Comptes-rendus des Journées Luxembourgeoises de Géodynamique, Bonn, Inst. f. Theoret. Geodäsie, vol. 80th session, no. 33, pp. 9-12, pp. B04102, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1996
    Keywords: Seismicity ; Geol. aspects ; Earthquake hazard
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    The 2002 Denali fault earthquake, Alaska: a large magnitude, slip-partitioned event (2003)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2003-05-17
    Description: The MW (moment magnitude) 7.9 Denali fault earthquake on 3 November 2002 was associated with 340 kilometers of surface rupture and was the largest strike-slip earthquake in North America in almost 150 years. It illuminates earthquake mechanics and hazards of large strike-slip faults. It began with thrusting on the previously unrecognized Susitna Glacier fault, continued with right-slip on the Denali fault, then took a right step and continued with right-slip on the Totschunda fault. There is good correlation between geologically observed and geophysically inferred moment release. The earthquake produced unusually strong distal effects in the rupture propagation direction, including triggered seismicity.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Eberhart-Phillips, Donna -- Haeussler, Peter J -- Freymueller, Jeffrey T -- Frankel, Arthur D -- Rubin, Charles M -- Craw, Patricia -- Ratchkovski, Natalia A -- Anderson, Greg -- Carver, Gary A -- Crone, Anthony J -- Dawson, Timothy E -- Fletcher, Hilary -- Hansen, Roger -- Harp, Edwin L -- Harris, Ruth A -- Hill, David P -- Hreinsdottir, Sigrun -- Jibson, Randall W -- Jones, Lucile M -- Kayen, Robert -- Keefer, David K -- Larsen, Christopher F -- Moran, Seth C -- Personius, Stephen F -- Plafker, George -- Sherrod, Brian -- Sieh, Kerry -- Sitar, Nicholas -- Wallace, Wesley K -- New York, N.Y. -- Science. 2003 May 16;300(5622):1113-8.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉U.S. Geological Survey, 4200 University Drive, Anchorage, AK 99508, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/12750512" 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
    Published by American Association for the Advancement of Science (AAAS)
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  • 4
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    Recurrent intraplate tectonism in the new madrid seismic zone (1980)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 1980-08-29
    Description: For the first time, New Madrid seismicity can be linked to specific structural features that have been reactivated through geologic time. Extensive seismic reflection profiling reveals major faults coincident with the main earthquake trends in the area and with structural deformation apparently caused by repeated episodes of igneous activity.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Zoback, M D -- Hamilton, R M -- Crone, A J -- Russ, D P -- McKeown, F A -- Brockman, S R -- New York, N.Y. -- Science. 1980 Aug 29;209(4460):971-6.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17747214" 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
    Published by American Association for the Advancement of Science (AAAS)
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  • 5
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    Surface Rupture and Slip Distribution of the Denali and Totschunda Faults (2005)
    Details
    Publication Date: 2017-04-04
    Description: The 3 November 2002 Denali fault, Alaska, earthquake resulted in 341 km of surface rupture on the Susitna Glacier, Denali, and Totschunda faults. The rupture proceeded from west to east and began with a 48-km-long break on the previously unknown Susitna Glacier thrust fault. Slip on this thrust averaged about 4 m (Crone et al., 2004). Next came the principal surface break, along 226 km of the Denali fault, with average right-lateral offsets of 4.5–5.1 m and a maximum offset of 8.8 m near its eastern end. The Denali fault trace is commonly left stepping and north side up. About 99 km of the fault ruptured through glacier ice, where the trace orientation was commonly influenced by local ice fabric. Finally, slip transferred southeastward onto the Totschunda fault and continued for another 66 km where dextral offsets average 1.6–1.8 m. The transition from the Denali fault to the Totschunda fault occurs over a complex 25-km-long transfer zone of right-slip and normal fault traces. Three methods of calculating average surface slip all yield a moment magnitude of Mw 7.8, in very good agreement with the seismologically determined magnitude of M 7.9. A comparison of strong-motion inversions for moment release with our slip distribution shows they have a similar pattern. The locations of the two largest pulses of moment release correlate with the locations of increasing steps in the average values of observed slip. This suggests that slipdistribution data can be used to infer moment release along other active fault traces.
    Description: Published
    Description: S23–S52
    Description: reserved
    Keywords: Surface Rupture ; Slip Distribution ; Denali fault ; Totschunda fault ; 3 November 2002 M 7.9 Earthquake ; Alaska ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 2137599 bytes
    Format: application/pdf
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  • 6
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    Paleoseismicity of Two Historically Quiescent Faults in Australia: Implications for Fault Behavior in Stable Continental Regions (2008)
    Seismological Society of America
    Details
    Publication Date: 2022-06-08
    Description: Paleoseismic studies of two historically aseismic Quaternary faults in Australia confirm that cratonic faults in stable continental regions (SCR) typically have a long-term behavior characterized by episodes of activity separated by quiescent intervals of at least 10,000 and commonly 100,000 years or more. Studies of the approximately 30-km-long Roopena fault in South Australia and the approximately 30-km-long Hyden fault in Western Australia document multiple Quaternary surface-faulting events that are unevenly spaced in time. The episodic clustering of events on cratonic SCR faults may be related to temporal fluctuations of fault-zone fluid pore pressures in a volume of strained crust. The long-term slip rate on cratonic SCR faults is extremely low, so the geomorphic expression of many cratonic SCR faults is subtle, and scarps may be difficult to detect because they are poorly preserved. Both the Roopena and Hyden faults are in areas of limited or no significant seismicity; these and other faults that we have studied indicate that many potentially hazardous SCR faults cannot be recognized solely on the basis of instrumental data or historical earthquakes. Although cratonic SCR faults may appear to be nonhazardous because they have been historically aseismic, those that are favorably oriented for movement in the current stress field can and have produced unexpected damaging earthquakes. Paleoseismic studies of modern and prehistoric SCR faulting events provide the basis for understanding of the long-term behavior of these faults and ultimately contribute to better seismic-hazard assessments.
    Description: Published
    Description: 1913-1934
    Description: 3.2. Tettonica attiva
    Description: JCR Journal
    Description: reserved
    Keywords: palaeoseismology ; Australia ; fault behavior ; stable continental regions ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 7
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    Holocene Behavior of the Brigham City Segment: Implications for Forecasting the Next Large-Magnitude Earthquake on the Wasatch Fault Zone, Utah (2012)
    Seismological Society of America (SSA)
    Details
    Publication Date: 2012-12-01
    Description: The Brigham City segment (BCS), the northernmost Holocene-active segment of the Wasatch fault zone (WFZ), is considered a likely location for the next big earthquake in northern Utah. We refine the timing of the last four surface-rupturing (~ M w  7) earthquakes at several sites near Brigham City (BE1, 2430±250; BE2, 3490±180; BE3, 4510±530; and BE4, B.P.) and calculate mean recurrence intervals (1060–1500 yr) that are greatly exceeded by the elapsed time (~2500 yr) since the most recent surface-rupturing earthquake (MRE). An additional rupture observed at the Pearsons Canyon site (PC1, B.P.) near the southern segment boundary is probably spillover rupture from a large earthquake on the adjacent Weber segment. Our seismic moment calculations show that the PC1 rupture reduced accumulated moment on the BCS about 22%, a value that may have been enough to postpone the next large earthquake. However, our calculations suggest that the segment currently has accumulated more than twice the moment accumulated in the three previous earthquake cycles, so we suspect that additional interactions with the adjacent Weber segment contributed to the long elapse time since the MRE on the BCS. Our moment calculations indicate that the next earthquake is not only overdue, but could be larger than the previous four earthquakes. Displacement data show higher rates of latest Quaternary slip (~1.3 mm/yr) along the southern two-thirds of the segment. The northern third likely has experienced fewer or smaller ruptures, which suggests to us that most earthquakes initiate at the southern segment boundary. Online Material: Cross sections, age estimates, evaluation of Box Elder delta earthquake chronology, code for OxCal models, trench logs, sources of surface offset data, and description of Call Fort gravel pit fault exposures.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
    Published by Seismological Society of America (SSA)
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  • 8
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    Late Quaternary Paleoseismology of the Southern Steens Fault Zone, Northern Nevada (2007)
    Seismological Society of America
    Details
    Publication Date: 2007-10-01
    Description: The 192-km-long Steens fault zone is the most prominent normal fault system in the northern Basin and Range province of western North America. We use trench mapping and radiometric dating to estimate displacements and timing of the last three surface-rupturing earthquakes (E1-E3) on the southern part of the fault south of Denio, Nevada. Coseismic displacements range from 1.1 to 2.2+ or -0.5 m, and radiometric ages indicate earthquake times of 11.5+ or -2.0 ka (E3), 6.1+ or -0.5 ka (E2), and 4.6+ or -1.0 ka (E1). These data yield recurrence intervals of 5.4+ or -2.1 k.y. between E3 and E2, 1.5+ or -1.1 k.y. between E2 and E1, and an elapsed time of 4.6+ or -1.0 k.y. since E1. The recurrence data yield variable interval slip rates (between 0.2+ or -0.22 and 1.5+ or -2.3 mm/yr), but slip rates averaged over the past approximately 18 k.y. (0.24+ or -0.06 mm/year) are similar to long-term (8.5-12.5 Ma) slip rates (0.2+ or -0.1 mm/yr) measured a few kilometers to the north. We infer from the lack of significant topographic relief across the fault in Bog Hot Valley that the fault zone is propagating southward and may now be connected with a fault at the northwestern end of the Pine Forest Range. Displacements documented in the trench and a rupture length of 37 km indicate a history of three latest Quaternary earthquakes with magnitudes of M 6.6-7.1 on the southern part of the Steens fault zone.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
    Published by Seismological Society of America
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  • 9
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    Defining the Southwestern End of the Blytheville Arch, Northeastern Arkansas: Delimiting a Seismic Source Zone in the New Madrid Region (1998)
    Seismological Society of America
    Details
    Publication Date: 1998-07-01
    Print ISSN: 0895-0695
    Electronic ISSN: 1938-2057
    Topics: Geosciences
    Published by Seismological Society of America
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  • 10
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    "The Geology of Earthquakes" by Robert S. Yeats, Kerry Sieh, and Clarence R. Allen (1997)
    Seismological Society of America
    Details
    Publication Date: 1997-09-01
    Print ISSN: 0895-0695
    Electronic ISSN: 1938-2057
    Topics: Geosciences
    Published by Seismological Society of America
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