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  • 1
    Publication Date: 2008-01-11
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Erren, Thomas C -- Reiter, Russel J -- Meyer-Rochow, V Benno -- England -- Nature. 2008 Jan 10;451(7175):127. doi: 10.1038/451127c.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18185565" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Cattle ; History, 20th Century ; Larva/drug effects ; Melatonin/*history/pharmacology ; Pineal Gland/chemistry ; Rana pipiens/*physiology ; *Skin Pigmentation/drug effects ; Tissue Extracts/pharmacology
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2012-03-03
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Meyer-Berthaud, Brigitte -- Decombeix, Anne-Laure -- England -- Nature. 2012 Feb 29;483(7387):41-2. doi: 10.1038/483041a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22382975" target="_blank"〉PubMed〈/a〉
    Keywords: *Biodiversity ; *Fossils ; Trees/*physiology
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 2012-01-06
    Description: From determining the optical properties of simple molecular crystals to establishing the preferred handedness in highly complex vertebrates, molecular chirality profoundly influences the structural, mechanical and optical properties of both synthetic and biological matter on macroscopic length scales. In soft materials such as amphiphilic lipids and liquid crystals, the competition between local chiral interactions and global constraints imposed by the geometry of the self-assembled structures leads to frustration and the assembly of unique materials. An example of particular interest is smectic liquid crystals, where the two-dimensional layered geometry cannot support twist and chirality is consequently expelled to the edges in a manner analogous to the expulsion of a magnetic field from superconductors. Here we demonstrate a consequence of this geometric frustration that leads to a new design principle for the assembly of chiral molecules. Using a model system of colloidal membranes, we show that molecular chirality can control the interfacial tension, an important property of multi-component mixtures. This suggests an analogy between chiral twist, which is expelled to the edges of two-dimensional membranes, and amphiphilic surfactants, which are expelled to oil-water interfaces. As with surfactants, chiral control of interfacial tension drives the formation of many polymorphic assemblages such as twisted ribbons with linear and circular topologies, starfish membranes, and double and triple helices. Tuning molecular chirality in situ allows dynamical control of line tension, which powers polymorphic transitions between various chiral structures. These findings outline a general strategy for the assembly of reconfigurable chiral materials that can easily be moved, stretched, attached to one another and transformed between multiple conformational states, thus allowing precise assembly and nanosculpting of highly dynamical and designable materials with complex topologies.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Gibaud, Thomas -- Barry, Edward -- Zakhary, Mark J -- Henglin, Mir -- Ward, Andrew -- Yang, Yasheng -- Berciu, Cristina -- Oldenbourg, Rudolf -- Hagan, Michael F -- Nicastro, Daniela -- Meyer, Robert B -- Dogic, Zvonimir -- R01 EB002583/EB/NIBIB NIH HHS/ -- England -- Nature. 2012 Jan 4;481(7381):348-51. doi: 10.1038/nature10769.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉The Martin Fisher School of Physics, Brandeis University, 415 South Street, Waltham, Massachusetts 02454, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22217941" target="_blank"〉PubMed〈/a〉
    Keywords: Amino Acid Substitution ; Bacteriophage M13/*chemistry/genetics ; Biomechanical Phenomena ; Colloids/chemistry ; Computer Simulation ; Microscopy, Electron, Transmission ; Oils/chemistry ; Stereoisomerism ; Surface Tension ; Surface-Active Agents/chemistry ; Water/chemistry
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2013-12-20
    Description: Dislocations represent one of the most fascinating and fundamental concepts in materials science. Most importantly, dislocations are the main carriers of plastic deformation in crystalline materials. Furthermore, they can strongly affect the local electronic and optical properties of semiconductors and ionic crystals. In materials with small dimensions, they experience extensive image forces, which attract them to the surface to release strain energy. However, in layered crystals such as graphite, dislocation movement is mainly restricted to the basal plane. Thus, the dislocations cannot escape, enabling their confinement in crystals as thin as only two monolayers. To explore the nature of dislocations under such extreme boundary conditions, the material of choice is bilayer graphene, the thinnest possible quasi-two-dimensional crystal in which such linear defects can be confined. Homogeneous and robust graphene membranes derived from high-quality epitaxial graphene on silicon carbide provide an ideal platform for their investigation. Here we report the direct observation of basal-plane dislocations in freestanding bilayer graphene using transmission electron microscopy and their detailed investigation by diffraction contrast analysis and atomistic simulations. Our investigation reveals two striking size effects. First, the absence of stacking-fault energy, a unique property of bilayer graphene, leads to a characteristic dislocation pattern that corresponds to an alternating AB B[Symbol: see text]AC change of the stacking order. Second, our experiments in combination with atomistic simulations reveal a pronounced buckling of the bilayer graphene membrane that results directly from accommodation of strain. In fact, the buckling changes the strain state of the bilayer graphene and is of key importance for its electronic properties. Our findings will contribute to the understanding of dislocations and of their role in the structural, mechanical and electronic properties of bilayer and few-layer graphene.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Butz, Benjamin -- Dolle, Christian -- Niekiel, Florian -- Weber, Konstantin -- Waldmann, Daniel -- Weber, Heiko B -- Meyer, Bernd -- Spiecker, Erdmann -- England -- Nature. 2014 Jan 23;505(7484):533-7. doi: 10.1038/nature12780. Epub 2013 Dec 18.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Center for Nanoanalysis and Electron Microscopy, Friedrich-Alexander-Universitat Erlangen-Nurnberg, Cauerstrasse 6, 91058 Erlangen, Germany. ; Interdisziplinares Zentrum fur Molekulare Materialien und Computer-Chemie-Centrum, Friedrich-Alexander-Universitat Erlangen-Nurnberg, Nagelsbachstrasse 25, 91052 Erlangen, Germany. ; Lehrstuhl fur Angewandte Physik, Friedrich-Alexander-Universitat Erlangen-Nurnberg, Staudtstrasse 7, 91058 Erlangen, Germany.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24352231" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 5
    Publication Date: 2015-06-18
    Description: West Africa is currently witnessing the most extensive Ebola virus (EBOV) outbreak so far recorded. Until now, there have been 27,013 reported cases and 11,134 deaths. The origin of the virus is thought to have been a zoonotic transmission from a bat to a two-year-old boy in December 2013 (ref. 2). From this index case the virus was spread by human-to-human contact throughout Guinea, Sierra Leone and Liberia. However, the origin of the particular virus in each country and time of transmission is not known and currently relies on epidemiological analysis, which may be unreliable owing to the difficulties of obtaining patient information. Here we trace the genetic evolution of EBOV in the current outbreak that has resulted in multiple lineages. Deep sequencing of 179 patient samples processed by the European Mobile Laboratory, the first diagnostics unit to be deployed to the epicentre of the outbreak in Guinea, reveals an epidemiological and evolutionary history of the epidemic from March 2014 to January 2015. Analysis of EBOV genome evolution has also benefited from a similar sequencing effort of patient samples from Sierra Leone. Our results confirm that the EBOV from Guinea moved into Sierra Leone, most likely in April or early May. The viruses of the Guinea/Sierra Leone lineage mixed around June/July 2014. Viral sequences covering August, September and October 2014 indicate that this lineage evolved independently within Guinea. These data can be used in conjunction with epidemiological information to test retrospectively the effectiveness of control measures, and provides an unprecedented window into the evolution of an ongoing viral haemorrhagic fever outbreak.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Carroll, Miles W -- Matthews, David A -- Hiscox, Julian A -- Elmore, Michael J -- Pollakis, Georgios -- Rambaut, Andrew -- Hewson, Roger -- Garcia-Dorival, Isabel -- Bore, Joseph Akoi -- Koundouno, Raymond -- Abdellati, Said -- Afrough, Babak -- Aiyepada, John -- Akhilomen, Patience -- Asogun, Danny -- Atkinson, Barry -- Badusche, Marlis -- Bah, Amadou -- Bate, Simon -- Baumann, Jan -- Becker, Dirk -- Becker-Ziaja, Beate -- Bocquin, Anne -- Borremans, Benny -- Bosworth, Andrew -- Boettcher, Jan Peter -- Cannas, Angela -- Carletti, Fabrizio -- Castilletti, Concetta -- Clark, Simon -- Colavita, Francesca -- Diederich, Sandra -- Donatus, Adomeh -- Duraffour, Sophie -- Ehichioya, Deborah -- Ellerbrok, Heinz -- Fernandez-Garcia, Maria Dolores -- Fizet, Alexandra -- Fleischmann, Erna -- Gryseels, Sophie -- Hermelink, Antje -- Hinzmann, Julia -- Hopf-Guevara, Ute -- Ighodalo, Yemisi -- Jameson, Lisa -- Kelterbaum, Anne -- Kis, Zoltan -- Kloth, Stefan -- Kohl, Claudia -- Korva, Misa -- Kraus, Annette -- Kuisma, Eeva -- Kurth, Andreas -- Liedigk, Britta -- Logue, Christopher H -- Ludtke, Anja -- Maes, Piet -- McCowen, James -- Mely, Stephane -- Mertens, Marc -- Meschi, Silvia -- Meyer, Benjamin -- Michel, Janine -- Molkenthin, Peter -- Munoz-Fontela, Cesar -- Muth, Doreen -- Newman, Edmund N C -- Ngabo, Didier -- Oestereich, Lisa -- Okosun, Jennifer -- Olokor, Thomas -- Omiunu, Racheal -- Omomoh, Emmanuel -- Pallasch, Elisa -- Palyi, Bernadett -- Portmann, Jasmine -- Pottage, Thomas -- Pratt, Catherine -- Priesnitz, Simone -- Quartu, Serena -- Rappe, Julie -- Repits, Johanna -- Richter, Martin -- Rudolf, Martin -- Sachse, Andreas -- Schmidt, Kristina Maria -- Schudt, Gordian -- Strecker, Thomas -- Thom, Ruth -- Thomas, Stephen -- Tobin, Ekaete -- Tolley, Howard -- Trautner, Jochen -- Vermoesen, Tine -- Vitoriano, Ines -- Wagner, Matthias -- Wolff, Svenja -- Yue, Constanze -- Capobianchi, Maria Rosaria -- Kretschmer, Birte -- Hall, Yper -- Kenny, John G -- Rickett, Natasha Y -- Dudas, Gytis -- Coltart, Cordelia E M -- Kerber, Romy -- Steer, Damien -- Wright, Callum -- Senyah, Francis -- Keita, Sakoba -- Drury, Patrick -- Diallo, Boubacar -- de Clerck, Hilde -- Van Herp, Michel -- Sprecher, Armand -- Traore, Alexis -- Diakite, Mandiou -- Konde, Mandy Kader -- Koivogui, Lamine -- Magassouba, N'Faly -- Avsic-Zupanc, Tatjana -- Nitsche, Andreas -- Strasser, Marc -- Ippolito, Giuseppe -- Becker, Stephan -- Stoecker, Kilian -- Gabriel, Martin -- Raoul, Herve -- Di Caro, Antonino -- Wolfel, Roman -- Formenty, Pierre -- Gunther, Stephan -- 095831/Wellcome Trust/United Kingdom -- England -- Nature. 2015 Aug 6;524(7563):97-101. doi: 10.1038/nature14594. Epub 2015 Jun 17.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉1] Public Health England, Porton Down, Wiltshire SP4 0JG, UK [2] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [3] University of Southampton, South General Hospital, Southampton SO16 6YD, UK. ; Department of Cellular and Molecular Medicine, School of Medical Sciences, University of Bristol, Bristol BS8 1TD, UK. ; Institute of Infection and Global Health, University of Liverpool, Liverpool L69 2BE, UK. ; Public Health England, Porton Down, Wiltshire SP4 0JG, UK. ; 1] Institute of Evolutionary Biology, University of Edinburgh, Edinburgh EH9 2FL, UK [2] Fogarty International Center, National Institutes of Health, Bethesda, Maryland 20892, USA [3] Centre for Immunology, Infection and Evolution, University of Edinburgh, Edinburgh EH9 2FL, UK. ; 1] Public Health England, Porton Down, Wiltshire SP4 0JG, UK [2] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [3] London School of Hygiene and Tropical Medicine, Keppel Street, London WC1E 7HT, UK. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Universite Gamal Abdel Nasser de Conakry, Laboratoire des Fievres Hemorragiques en Guinee, Conakry, Guinea [3] Institut National de Sante Publique, Conakry, Guinea. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Institute of Tropical Medicine, B-2000 Antwerp, Belgium. ; 1] Public Health England, Porton Down, Wiltshire SP4 0JG, UK [2] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Institute of Lassa Fever Research and Control, Irrua Specialist Teaching Hospital, Irrua, Edo State, Nigeria. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Bernhard Nocht Institute for Tropical Medicine, D-20359 Hamburg, Germany [3] German Centre for Infection Research (DZIF), 38124 Braunschweig, Germany. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Swiss Tropical and Public Health Institute, University of Basel, CH-4002 Basel, Switzerland. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Bernhard Nocht Institute for Tropical Medicine, D-20359 Hamburg, Germany. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] German Centre for Infection Research (DZIF), 38124 Braunschweig, Germany [3] Institute of Virology, Philipps University Marburg, 35043 Marburg, Germany. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] National Reference Center for Viral Hemorrhagic Fevers, 69365 Lyon, France [3] Laboratoire P4 Inserm-Jean Merieux, US003 Inserm, 69365 Lyon, France. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Department of Biology, University of Antwerp, B-2020 Antwerp, Belgium. ; 1] Public Health England, Porton Down, Wiltshire SP4 0JG, UK [2] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [3] Institute of Infection and Global Health, University of Liverpool, Liverpool L69 2BE, UK. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Robert Koch Institute, 13353 Berlin, Germany. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] National Institute for Infectious Diseases (INMI) Lazzaro Spallanzani, 00149 Rome, Italy. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] German Centre for Infection Research (DZIF), 38124 Braunschweig, Germany [3] Friedrich Loeffler Institute, Federal Research Institute for Animal Health, 17493 Greifswald, Insel Riems, Germany. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Bernhard Nocht Institute for Tropical Medicine, D-20359 Hamburg, Germany [3] KU Leuven Rega institute, B-3000 Leuven, Belgium. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Bernhard Nocht Institute for Tropical Medicine, D-20359 Hamburg, Germany [3] Redeemer's University, Osun State, Nigeria. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Centro Nacional de Microbiologia, Instituto de Salud Carlos III, 28029 Madrid, Spain. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] National Reference Center for Viral Hemorrhagic Fevers, 69365 Lyon, France [3] Unite de Biologie des Infections Virales Emergentes, Institut Pasteur, 69365 Lyon, France. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] German Centre for Infection Research (DZIF), 38124 Braunschweig, Germany [3] Bundeswehr Institute of Microbiology, 80937 Munich, Germany. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] National Center for Epidemiology, National Biosafety Laboratory, H-1097 Budapest, Hungary. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Institute of Microbiology and Immunology, Faculty of Medicine, University of Ljubljana, SI-1000 Ljubljana, Slovenia. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Public Health Agency of Sweden, 171 82 Solna, Sweden. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] German Centre for Infection Research (DZIF), 38124 Braunschweig, Germany [3] Heinrich Pette Institute - Leibniz Institute for Experimental Virology, 20251 Hamburg, Germany. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] KU Leuven Rega institute, B-3000 Leuven, Belgium. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] German Centre for Infection Research (DZIF), 38124 Braunschweig, Germany [3] Institute of Virology, University of Bonn, 53127 Bonn, Germany. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Federal Office for Civil Protection, Spiez Laboratory, CH-3700 Spiez, Switzerland. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Bundeswehr Hospital, 22049 Hamburg, Germany. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Institute of Virology and Immunology, CH-3147 Mittelhausern, Switzerland. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Janssen-Cilag, SE-192 07 Sollentuna, Sweden. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Thunen Institute, D-22767 Hamburg, Germany. ; Eurice - European Research and Project Office GmbH, 10115 Berlin, Germany. ; Centre for Genomic Research, Institute of Integrative Biology, University of Liverpool, Liverpool L69 7ZB, UK. ; Institute of Evolutionary Biology, University of Edinburgh, Edinburgh EH9 2FL, UK. ; Department of Infection and Population Health, University College London, London WC1E 6JB, UK. ; Research IT, University of Bristol, Bristol BS8 1HH, UK. ; Advanced Computing Research Centre, University of Bristol, Bristol BS8 1HH, UK. ; Ministry of Health Guinea, Conakry, Guinea. ; World Health Organization, 1211 Geneva 27, Switzerland. ; World Health Organization, Conakry, Guinea. ; Medecins Sans Frontieres, B-1050 Brussels, Belgium. ; Section Prevention et Lutte contre la Maladie a la Direction Prefectorale de la Sante de Gueckedou, Gueckedou, Guinea. ; Universite Gamal Abdel Nasser de Conakry, CHU Donka, Conakry, Guinea. ; Health and Sustainable Development Foundation, Conakry, Guinea. ; Institut National de Sante Publique, Conakry, Guinea. ; Universite Gamal Abdel Nasser de Conakry, Laboratoire des Fievres Hemorragiques en Guinee, Conakry, Guinea. ; 1] The European Mobile Laboratory Consortium, Bernhard-Nocht-Institute for Tropical Medicine, D-20359 Hamburg, Germany [2] Laboratoire P4 Inserm-Jean Merieux, US003 Inserm, 69365 Lyon, France.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26083749" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 6
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We have studied the Cenozoic and active tectonics of the north-eastern rim of Tibet west of the Yellow River (Gansu, China) where the western Haiyuan Fault enters the eastern Qilian Shan, a high mountainous region, which was the site of the 1927 May 23, M= 8-8.3, Gulang earthquake. Fieldwork, combined with analysis of aerial photographs and satellite images, reveals consistent cumulative left-lateral offsets of postglacial geomorphic features along the fault, but no recent rupture. West of the Tianzhu pull-apart basin, the levelling of offset-terrace risers implies Holocene horizontal and vertical slip rates on the steeply south-dipping, N110E-striking fault of 11 ± 4 and 1.3 ± 0.3 mm yr-1, respectively. The presence of subordinate, mostly normal, throws due to local changes in fault strike, and kinematic compatibility at the SW corner of the Tianzhu basin, constrains the azimuth of the fault-slip vector to be N110-115E. On the less prominent, N85-100E-striking Gulang Fault, which splays eastwards from the Haiyuan Fault near 102.2°E, less detailed observations suggest that the average Holocene left-slip rate is 4.3 ± 2.1 mm yr-1 with a minor component of ˜˜N-directed thrusting, with no recent seismic break either. East of ˜˜103°E, coeval slip on both faults thus appears to account for as much as 15 ± 6 mm yr-1 of left-lateral movement between NE Tibet and the southern edge of the Ala Shan Platform, in a N105 ± 6E direction. West of ˜˜103°E structural and geomorphic evidence implies that ˜˜NNE-directed shortening of that edge across the rising, north-eastern Qilian mountain ranges occurs at a rate of 4 ± 2 mm yr-1, by movement on right-stepping thrusts that root on a 10-20°S-dipping décollement that probably branches off the Haiyuan Fault at a depth of ˜˜25 km. The existence of fresh surface breaks with metre-high free faces on a N-dipping, hanging-wall normal fault south of the easternmost, Dongqingding thrust segment, and of half-metre-high pressure ridges on that segment, indicates that the 1927 Gulang earthquake ruptured that complex thrust system. The ˜˜4 mm yr-1 shortening rate is consistent with the inference that the thrusts formed and move as a result of orthogonal slip partitioning in a large restraining bend of the Haiyuan Fault.Based on a retrodeformable structural section, we estimate the cumulative shortening on the Qilian Shan thrusts, north of the Haiyuan Fault, to be at least 25 km. The finite displacements and current slip rates on either the thrusts or the left-lateral faults imply that Cenozoic deformation started in the Late Miocene, with slip partitioning during much of the Plio-Quaternary. Assuming coeval slip at the present rates on the Haiyuan and Gulang Faults in the last 8 Ma would bring the cumulative left-lateral displacement between NE Tibet and the Ala Shan Platform to about 120 km, consistent with the 95 ± 15 km offset of the Yellow River across the Haiyuan Fault, but many times the offset (˜˜16 km) inferred on one rccent strand of that fault east of the river. Relative to the SE Gobi Desert, NE Tibet thus appears to have moved by a fair amount in the Late Cenozoic and is still moving fast. While some of this motion probably contributes to displace (towards the ESE) and rotate (CCW) the south-west edge of the Ordos block, much of it appears to be transmitted to the South China block, which leads, with the additional contribution of other large left-slip faults to the south and despite thrusting in the Lungmen Shan, to the extrusion (towards the ESE-SE) of that block relative to the Gobi, hcncc to north-eastern Asia.The ˜˜260 km long western Haiyuan Fault links two faults that ruptured about 70 years ago during two great earthquakes only seven years apart. Despite spectacular evidence of Holocene movement, it bears no trace of a large earthquake in the past eight centuries, either in the field or in the historical record. Given its relatively high slip rate, it should therefore be singled out as one of the most critical sites for impending great earthquakes (at least M ≥ 7.5, probably M ≥ 8) in the region. That such a seismic gap, called here the ‘Tianzhu gap', lies only ˜˜100 km north of Lanzhou and Xining, largest population centres of west-central China, makes instrumental monitoring of that fault particularly urgent. That the M ˜˜ 8, Gulang earthquake ruptured a complex thrust surface under high mountains in a restraining bend of the Haiyuan strike-slip fault suggests that the occurrence of comparable earthquakes in other areas with similar fault geometry, such as south of the big bend of the San Andreas Fault in California, should not be ruled out.
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 126 (1996), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We present geological and morphological observations at different scales to constrain rates of faulting and the distribution of deformation in the seismically active Aegean region. We focus first on the 130 km long Corinth Rift, an asymmetric graben where a flight of terraces of marine origin are uplifted. We show that the edges of the terraces lie in the footwall of the normal fault bounding the Corinth Rift and correspond to sea-level highstands of laic Pleistocene age. Using a detailed analysis of aerial and SPOT imagery supported by field observations, we have mapped 10 terrace platforms and strandlines ranging in elevation from 10 to 400 m over distances of 2 to 20 km from the fault. The elevation of the terraces' inner edges was estimated at 172 sites with an error of ±5m. This data set contains a precise description of the uplift and flexure of 10 different palaeohorizontal lines with respect to the present sea level. To date the deformation, we correlate the Corinth terraces with late Pleistocene oxygen-isotope stages of high sea-level stands and with global sea-level fluctuations. Using a thick elastic plate model consistent with our current understanding of the earthquake cycle and a boundary-element technique we reproduce the geometry of the shorelines to constrain both mechanical parameters and the slip on the fault. We show that the seismogenic layer behaves over the long term as if its elastic modulus were reduced by a factor of about 1000. All the terraces are fitted for fault slip increasing in proportion to terrace age, and the component of regional uplift is found to be less than 0.3 mm yr−1. The best fits give a slip rate of 11±3 mm yr−1 on the main rift-bounding fault over the last 350 kyr. Other geological and morphologic information allows us to estimate the total age of the main fault (∼1 Ma) and to examine the mechanical evolution of the Corinth Rift. The minimum observed sediment thickness in the Gulf places an extreme check on the results of the modelling and a lower bound on slip rate of 6–7 mm yr−1 (40 per cent less than estimated with modelling). Even this slip rate is nearly 10 times higher than for comparable features in most of the Aegean and elsewhere in the world.At a larger scale, the spacing and asymmetry of the rift systems in the Aegean suggest strain localization in the upper mantle, with slow extension starting 15 Myr ago or earlier. The more recent (1 Myr), rapid phase of rifting in Corinth partly reactivated this earlier phase of extension. The younger faulting in Corinth appears to result from its present location in the inhomogeneous stress field (process zone) of the south-westward propagating tip of the southern branch of the North Anatolian Fault. We extend these relations to propose a mechanical model for the Late Cenozoic evolution of the Aegean. As the Arabia/Europe collision progressed in eastern Turkey it caused Anatolia to move to the west and the North Anatolian Fault to propagate into the Aegean, where the early slow extension started to be modified about 5 Ma ago. The process of propagation dramatically increased the activity of some but not all of the earlier rifts. The model we present is compatible with tectonic observations, as well as with the seismicity, the palaeomagnetic rotations and the displacement field now observed with GPS and SLR.
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 124 (1996), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Field work carried out in Gansu province and complemented with analysis of SPOT panchromatic scenes allows us to characterize the deformations along the eastern segment of the Altyn Tagh fault and to place bounds on its Holocene left slip rate. East of 96°E, the long-term, left-lateral offset of stream channels, alluvial fans, and terrace edges is about 50 m. These offsets are most probably of Holocene age (12 ± 2 ka) and imply that the corresponding derived slip rate is 4 ± 2 mm yr−1. This observation is consistent with a north-eastward along-strike decreasing slip rate on the Altyn fault due to partitioning of slip on multiple, more easterly trending splays.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 511 (1987), S. 0 
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 405 (1983), S. 0 
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
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