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  • 1
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    In:  Geophys. Res. Lett., Edmonton, Conseil de l'Europe, vol. 24, no. 23, pp. 3081-3084, pp. B10410, (ISSN: 1340-4202)
    Publication Date: 1997
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Fault zone ; Tectonics ; 7230 ; Seismology ; Seismicity ; and ; seismotectonics ; Seismology ; 8010 ; Structural ; geology ; 8165 ; Fractures ; and ; faults ; 7221 ; Paleoseismology ; 7209 ; GRL ; Earthquake ; dynamics ; and ; mechanics
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  • 2
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    In:  J. Struct. Geol., Edmonton, Conseil de l'Europe, vol. 23, no. 2-3, pp. 473-487, pp. B10410, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Stress ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Structural geology ; Fault plane solution, focal mechanism ; Fault zone ; JSG
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  • 3
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    In:  J. Geodynamics, Warszawa, Inst. Electrical & Electronics Engineers, vol. 26, no. 2-4, pp. 461-468, pp. 1496, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1998
    Keywords: Fault zone ; Earthquake ; Strain ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; blocks ; Fracture
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  • 4
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    In:  Tectonophys., Bonn, Inst. f. Theoret. Geodäsie, vol. 408, no. 1-4, pp. 147-176, pp. B05318, (ISSN: 1340-4202)
    Publication Date: 2005
    Keywords: paleo ; Seismicity ; Geol. aspects ; Earthquake hazard ; Deformation ; rates ; Global Positioning System ; Paleoseismology ; Scarp ; profiles ; Seismic ; hazard ; assessment ; Crustal deformation (cf. Earthquake precursor: deformation or strain)
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  • 5
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    In:  Journal of Structural Geology, Tokyo, Lawrence Livermore National Laboratory, vol. 18, no. 1-2, pp. 835-845, pp. L11604, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Fault zone ; Fracture ; Geol. aspects ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Structural geology ; JSG
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  • 6
    Publication Date: 2019
    Description: Abstract Preserved sets of marine terraces and palaeoshorelines above subduction zones provide an opportunity to explore the long‐term deformation that occurs as a result of upper‐plate extension. We investigate uplifted palaeoshorelines along the South Central Crete Fault (SCCF) and over its western tip, located above the Hellenic Subduction Zone, in order to derive uplift rates and examine the role that known extensional faults contribute to observed coastal uplift. We have mapped palaeoshorelines and successfully dated four Late‐Quaternary wave‐cut platforms using in‐situ 36Cl exposure dating. These absolute ages are used to guide a correlation of palaeoshorelines with Quaternary sea‐level highstands from 76.5 to ~900 ka; the results of which suggest that uplift rates vary along fault strikes but have been constant for up to 600 ka in places. Correlation of palaeoshorelines across the SCCF results in a throw‐rate of 0.41 mm/yr and, assuming repetition of 1.1 m slip events, a fault‐specific earthquake recurrence interval of approximately 2700 years. Elastic‐half space modelling implies that coastal uplift is related to offshore upper‐plate extensional faults. These faults may be responsible for perturbing the uplift rate signals in the south central Crete area. Our findings suggest that where uplifted marine terraces are used to make inferences about the mechanisms responsible for uplift throughout the Hellenic Subduction Zone, and other subduction zones worldwide, the impact of upper‐plate extensional faults over multiple seismic cycles should also be considered.
    Print ISSN: 0278-7407
    Electronic ISSN: 1944-9194
    Topics: Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 7
    Publication Date: 2019
    Electronic ISSN: 2045-2322
    Topics: Natural Sciences in General
    Published by Springer Nature
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  • 8
    Publication Date: 2011-04-19
    Description: The transient response of bedrock rivers to a drop in base level can be used to discriminate between competing fluvial erosion models. However, some recent studies of bedrock erosion conclude that transient river long profiles can be approximately characterized by a transport-limited erosion model, while other authors suggest that a detachment-limited model best explains their field data. The difference is thought to be due to the relative volume of sediment being fluxed through the fluvial system. Using a pragmatic approach, we address this debate by testing the ability of end-member fluvial erosion models to reproduce the well-documented evolution of three catchments in the central Apennines (Italy) which have been perturbed to various extents by an independently constrained increase in relative uplift rate. The transport-limited model is unable to account for the catchments' response to the increase in uplift rate, consistent with the observed low rates of sediment supply to the channels. Instead, a detachment-limited model with a threshold corresponding to the field-derived median grain size of the sediment plus a slope-dependent channel width satisfactorily reproduces the overall convex long profiles along the studied rivers. Importantly, we find that the prefactor in the hydraulic scaling relationship is uplift dependent, leading to landscapes responding faster the higher the uplift rate, consistent with field observations. We conclude that a slope-dependent channel width and an entrainment/erosion threshold are necessary ingredients when modeling landscape evolution or mapping the distribution of fluvial erosion rates in areas where the rate of sediment supply to channels is low.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 9
    Publication Date: 2011-06-01
    Description: Sugar molecules adsorbed at hydrated inorganic oxide surfaces occur ubiquitously in nature and in technologically important materials and processes, including marine biomineralization, cement hydration, corrosion inhibition, bioadhesion, and bone resorption. Among these examples, surprisingly diverse hydration behaviors are observed for oxides in the presence of saccharides with closely related compositions and structures. Glucose, sucrose, and maltodextrin, for example, exhibit significant differences in their adsorption selectivities and alkaline reaction properties on hydrating aluminate, silicate, and aluminosilicate surfaces that are shown to be due to the molecular architectures of the saccharides. Solid-state 1H, 13C, 29Si, and 27Al nuclear magnetic resonance (NMR) spectroscopy measurements, including at very high magnetic fields (19 T), distinguish and quantify the different molecular species, their chemical transformations, and their site-specific adsorption on different aluminate and silicate moieties. Two-dimensional NMR results establish nonselective adsorption of glucose degradation products containing carboxylic acids on both hydrated silicates and aluminates. In contrast, sucrose adsorbs intact at hydrated silicate sites and selectively at anhydrous, but not hydrated, aluminate moieties. Quantitative surface force measurements establish that sucrose adsorbs strongly as multilayers on hydrated aluminosilicate surfaces. The molecular structures and physicochemical properties of the saccharides and their degradation species correlate well with their adsorption behaviors. The results explain the dramatically different effects that small amounts of different types of sugars have on the rates at which aluminate, silicate, and aluminosilicate species hydrate, with important implications for diverse materials and applications.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 10
    Publication Date: 2013-11-29
    Description: Nature Geoscience 6, 1036 (2013). doi:10.1038/ngeo1991 Authors: P. A. Cowie, C. H. Scholz, G. P. Roberts, J. P. Faure Walker & P. Steer Viscous flow in the deep crust and uppermost mantle can contribute to the accumulation of strain along seismogenic faults in the shallower crust. It is difficult to evaluate this contribution to fault loading because it is unclear whether the viscous deformation occurs in localized shear zones or is more broadly distributed. Furthermore, the rate of strain accumulation by viscous flow has a power law dependence on the stress applied, yet there are few direct estimates of what the power law exponent is, over the long term, for active faults. Here we measure topography and the offset along fault surfaces created during successive episodes of slip on seismically active extensional faults in the Italian Apennines during the Holocene epoch. We show that these data can be used to derive a relationship between the stress driving deformation and the fault strain rate, averaged over about 15 thousand years (kyr). We find that this relationship follows a well-defined power law with an exponent in the range of 3.0–3.3 (1σ). This exponent is consistent with nonlinear viscous deformation in the deep crust and, crucially, strain localization promoted by seismogenic faulting at shallower depths. Although we cannot rule out some distributed deformation, we suggest that fault strain and thus earthquake recurrence in the Apennines is largely controlled by viscous flow in deep, localized shear zones, over many earthquake cycles.
    Print ISSN: 1752-0894
    Electronic ISSN: 1752-0908
    Topics: Geosciences
    Published by Springer Nature
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