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  • 1
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    In:  Geophys. Res. Lett., Warszawa, Elsevier, vol. 32, no. 2, pp. 984-1002, pp. L02307, (ISBN: 0-12-018847-3)
    Publication Date: 2005
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Earthquake ; GRL
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  • 2
    Publication Date: 2016-06-21
    Description: The occurrence of large earthquakes in stable continental interiors challenges the applicability of the classical steady-state ‘seismic cycle’ model to such regions. Here, we shed new light onto this issue using as a case study the cluster of large reverse faulting earthquakes that occurred in Fennoscandia at 11-9 ka, triggered by the removal of the ice load during the final phase of regional deglaciation. We show that these reverse-faulting earthquakes occurred at a time when the horizontal strain-rate field was extensional, which implies that these events did not release horizontal strain that was building up at the time, but compressional strain that had been accummulated and stored elastically in the lithosphere over timescales similar to or longer than a glacial cycle. We argue that the tectonically-stable continental lithosphere can store elastic strain on long timescales, the release of which may be triggered by rapid, local transient stress changes caused by surface mass redistribution, resulting in the occurrence of intermittent intraplate earthquakes.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 3
    Publication Date: 2013-02-01
    Description: Nature Geoscience 6, 152 (2013). doi:10.1038/ngeo1720 Authors: S. N. Sapkota, L. Bollinger, Y. Klinger, P. Tapponnier, Y. Gaudemer & D. Tiwari
    Print ISSN: 1752-0894
    Electronic ISSN: 1752-0908
    Topics: Geosciences
    Published by Springer Nature
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  • 4
    Publication Date: 2016-01-29
    Description: In 1255, 1344, and 1408 AD, then again in 1833, 1934, and 2015, large earthquakes, devastated Kathmandu. The 1255 and 1934 surface ruptures have been identified east of the city, along comparable segments of the Main Frontal Thrust (MFT). Whether the other two pairs of events were similar is unclear. Taking into account charcoal’s age inheritance, we revisit the timing of terrace offsets at key sites to compare them with the seismic record since 1200 AD. The location, extent, and moment of the 1833 and 2015 events imply that they released only a small part of the regional slip deficit on a deep thrust segment that stopped north of the Siwaliks. By contrast, the 1344 or 1408 AD earthquake may have ruptured the MFT up to the surface in central Nepal between Kathmandu and Pokhara, east of the surface trace of the great 1505 AD earthquake which affected western Nepal. If so, the whole megathrust system in Nepal broke in a sequence of earthquakes that lasted less than three centuries, with ruptures that propagated up to the surface from east to west. Today’s situation in the Himalayan seismic sequence might be close to that of the fourteenth century.
    Print ISSN: 1343-8832
    Electronic ISSN: 1880-5981
    Topics: Geosciences
    Published by SpringerOpen
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  • 5
    Publication Date: 2014-06-06
    Description: On 28–29 October 2008, within twelve hours, two similar Mw = 6.4 strike-slip earthquakes struck Baluchistan (Pakistan), as part of a complex seismic sequence. Interferometric Synthetic Aperture Radar (InSAR) data reveal that the peak of surface displacement is near the Ziarat anticline, a large active fold affected by Quaternary strike-slip faulting. All coseismic interferograms integrate the deformation due to both earthquakes. As their causative faults ruptured close to each other, the individual signals cannot be separated. According to their focal mechanisms, each earthquake may have activated a NE-SW sinistral or a NW-SE dextral fault segment, which leads to four possible scenarios of fault orientations. A non-linear inversion of the InSAR dataset allows rejecting two scenarios. The best slip distributions on the two fault segments for the two remaining scenarios are determined by linear inversion. Stress-change modelling favours a scenario involving two abutting conjugate strike-slip faults. Two other fault segments accommodated left-lateral strike slip during the seismic sequence. The activated fault system includes multiple fault segments with different orientations and little surface expression. This may highlight, at a smaller scale, the distributed, possibly transient character of deformation within a broader right-lateral shear zone. It suggests that the activated faults delineate a small tectonic block extruding and subtly rotating within the shear zone. It occurs in the vicinity of the local tectonic syntaxis where orogenic structures sharply turn around a vertical axis. These mechanisms could participate in the long-term migration of active tectonic structures within this kinematically unstable tectonic syntaxis.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 6
    Publication Date: 2014-08-08
    Description: ABSTRACT The return times of large Himalayan earthquakes are poorly constrained. Despite historical devastation of cities along the mountain range, definitive links between events and specific segments of the Main Frontal Thrust (MFT) are not established, and paleo-seismological records have not documented the occurrence of several similar events at the same location. In east-central Nepal, however, recently discovered primary surface ruptures of that mega-thrust in the AD 1255 and 1934 earthquakes are associated with flights of tectonically uplifted terraces. We present here a refined, longer slip history of the MFT's two overlapping strands (Patu and Bardibas Thrusts) in that region, based on updated geomorphic/neo-tectonic mapping of active faulting, two 1.3 km-long shallow seismic profiles, and logging of 2 rivercut cliffs, 3 paleo-seismological trenches and several pits, with constraints from 74 detrital charcoals and 14 cosmogenic nuclide ages. The amount of hanging-wall uplift on the Patu thrust since 3650 ± 450 years requires 3 more events than the two aforementioned. The uplift rate (8.5 ± 1.5 mm/yr), thrust dip (25° ± 5 °N) and apparent characteristic behavior imply 12–17.5 m of slip per event. On the Bardibas thrust, discrete pulses of colluvial deposition resulting from the co-seismic growth of a flexural fold scarp suggest the occurrence of 6 or 7 paleo-earthquakes in the last 4500 ± 50 years. The coeval rupture of both strands during great Himalayan earthquakes implies that, in Eastern Nepal, the Late Holocene return times of such earthquakes probably ranged between 750 ± 140 and 870 ± 350 years.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 7
    Publication Date: 2001-06-26
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Schwartlander, B -- Stover, J -- Walker, N -- Bollinger, L -- Gutierrez, J P -- McGreevey, W -- Opuni, M -- Forsythe, S -- Kumaranayake, L -- Watts, C -- Bertozzi, S -- New York, N.Y. -- Science. 2001 Jun 29;292(5526):2434-6. Epub 2001 Jun 21.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Joint United Nations Programme on HIV/AIDS (UNAIDS), Geneva, Switzerland. schwartlanderb@unaids.org〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/11423619" target="_blank"〉PubMed〈/a〉
    Keywords: Acquired Immunodeficiency Syndrome/*economics/epidemiology/prevention & ; control/therapy ; Africa South of the Sahara ; Antiretroviral Therapy, Highly Active ; Developed Countries/economics ; Developing Countries/economics ; Female ; Financing, Organized ; *Global Health ; HIV Infections/*economics/epidemiology/prevention & control/therapy ; Health Care Costs ; *Health Expenditures ; *Health Resources ; Health Services/economics ; Humans ; International Cooperation ; Male ; Private Sector ; Public Sector ; United Nations
    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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  • 8
    Publication Date: 2015-08-08
    Description: Detailed geodetic imaging of earthquake ruptures enhances our understanding of earthquake physics and associated ground shaking. The 25 April 2015 moment magnitude 7.8 earthquake in Gorkha, Nepal was the first large continental megathrust rupture to have occurred beneath a high-rate (5-hertz) Global Positioning System (GPS) network. We used GPS and interferometric synthetic aperture radar data to model the earthquake rupture as a slip pulse ~20 kilometers in width, ~6 seconds in duration, and with a peak sliding velocity of 1.1 meters per second, which propagated toward the Kathmandu basin at ~3.3 kilometers per second over ~140 kilometers. The smooth slip onset, indicating a large (~5-meter) slip-weakening distance, caused moderate ground shaking at high frequencies (〉1 hertz; peak ground acceleration, ~16% of Earth's gravity) and minimized damage to vernacular dwellings. Whole-basin resonance at a period of 4 to 5 seconds caused the collapse of tall structures, including cultural artifacts.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Galetzka, J -- Melgar, D -- Genrich, J F -- Geng, J -- Owen, S -- Lindsey, E O -- Xu, X -- Bock, Y -- Avouac, J-P -- Adhikari, L B -- Upreti, B N -- Pratt-Sitaula, B -- Bhattarai, T N -- Sitaula, B P -- Moore, A -- Hudnut, K W -- Szeliga, W -- Normandeau, J -- Fend, M -- Flouzat, M -- Bollinger, L -- Shrestha, P -- Koirala, B -- Gautam, U -- Bhatterai, M -- Gupta, R -- Kandel, T -- Timsina, C -- Sapkota, S N -- Rajaure, S -- Maharjan, N -- New York, N.Y. -- Science. 2015 Sep 4;349(6252):1091-5. doi: 10.1126/science.aac6383. Epub 2015 Aug 6.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Geology and Planetary Sciences, California Institute of Technology (Caltech), Pasadena, CA 91125, USA. ; BerkeleySeismological Laboratory, University of California (UC)-Berkeley, Berkeley, CA 94720, USA. ; Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, UC-San Diego, La Jolla, CA 92037, USA. ; Jet Propulsion Laboratory (JPL), Caltech, Pasadena, CA 91109, USA. ; Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK. Department of Geology and Planetary Sciences, California Institute of Technology (Caltech), Pasadena, CA 91125, USA. ; Department of Mines and Geology, Lainchour, Kathmandu, Nepal. ; Nepal Academy of Science and Technology, Khumaltar, Lalitpur, Nepal. ; Department of Geological Sciences, Central Washington University (CWU), Ellensberg, WA 98926, USA. ; Tri-Chandra Campus, Tribhuvan University, Ghantaghar, Kathmandu, Nepal. ; U.S. Geological Survey (USGS), Pasadena, CA 91106, USA. ; Pacific Northwest Geodetic Array and Department of Geological Sciences, CWU, Ellensberg, WA 98926, USA. ; UNAVCO, Boulder, CO 80301, USA. ; Departement Analyse et Sureveillance de l'Environnement (DASE), Commissariat a l'Energie Atomique (CEA), 91297 Bruyeres-le-Chatel, Arpajon, France.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26249228" 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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  • 9
    Publication Date: 2012-12-22
    Description: Nature Geoscience 6, 71 (2013). doi:10.1038/ngeo1669 Authors: S. N. Sapkota, L. Bollinger, Y. Klinger, P. Tapponnier, Y. Gaudemer & D. Tiwari
    Print ISSN: 1752-0894
    Electronic ISSN: 1752-0908
    Topics: Geosciences
    Published by Springer Nature
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  • 10
    Publication Date: 2019
    Description: Abstract The Charnath Khola is a large river crossing the Himalayan thrust system in the region devastated by the great M 8.3 1934 Bihar‐Nepal earthquake. Fluvial terraces are abandoned along the river and at the base of a ~20 m‐high cumulative thrust escarpment. A trench across the fault scarp exposed Siwalik mudstone/siltstone overthrusting Quaternary units and three colluvial wedges interfingered with fluvial sands. 85 AMS radiocarbon dates, from detrital charcoals sampled in the trench, a rivercut and river terraces, constrain the timing of the sedimentary processes following the last two major earthquakes, in 1934 and 1255 CE. Although several samples straddle the main earthquake horizon, associating it with the 1934 earthquake, based solely on radiocarbon ages, remains challenging. The 49 detrital charcoal ages found in the pre‐ and post‐earthquake units fall between 65 BP and 225 BP, a period with a flat calibration curve. Many of these radiocarbon ages are suspected to include a part due to inbuilt time (i.e., age of the wood at the time of burning), transport time, and reworking processes, which are difficult to resolve. Considering these ages at their face value could lead to dates older than the actual earthquake dates. We suggest that a part of this chronological bias is also related to a local post‐seismic aggradation pulse of 4 to 5 metres of sediments, which is documented in the trench and terraces. This fluvial sequence, hiding the most recent surface rupture, is likely related to landslide‐sediment deposition triggered by the 1934 Bihar‐Nepal earthquake.
    Print ISSN: 2169-9313
    Electronic ISSN: 2169-9356
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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