Zobrazeno 1 - 10 of 36 pro vyhledávání: '"A. Druiventak"'
1
Akademický článek
Experimental deformation and recrystallization of olivine – processes and timescales of damage healing during postseismic relaxation at mantle depths
Autor: C. A. Trepmann, J. Renner, A. Druiventak
Publikováno v: Solid Earth, Vol 4, Iss 2, Pp 423-450 (2013)
Experiments comprising sequences of deformation (at 300 or 600 °C) and annealing at varying temperature (700 to 1100 °C), time (up to 144 h) and stress (up to 1.5 GPa) were carried out in a Griggs-type apparatus on natural olivine-rich peridotite s
Externí odkaz: https://doaj.org/article/ae873a8cde56460d83d742bd64c1ffee
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3
Akademický článek
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4
Crystallographic preferred orientations may develop in nanocrystalline materials on fault planes due to surface energy interactions
Autor: Virginia Toy, Anthony Druiventak, Richard Wirth, Thomas M. Mitchell
Publikováno v: Geochemistry, Geophysics, Geosystems. 16:2549-2563
A layer of substantially noncrystalline material, composed of partially annealed nanopowder with local melt, was experimentally generated by comminution during ∼1.5 mm total slip at ∼2.5 × 10−6 m s−1, Pconf ∼ 0.5 GPa, and 450°C or 600°C,
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::32c20fb777e330f5a2f5c8e9e0f6898a
https://doi.org/10.1002/2015gc005857
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5
Experimental deformation and recrystallization of olivine – processes and timescales of damage healing during postseismic relaxation at mantle depths
Autor: Anthony Druiventak, Jörg Renner, Claudia A. Trepmann
Publikováno v: Solid Earth, Vol 4, Iss 2, Pp 423-450 (2013)
Experiments comprising sequences of deformation (at 300 or 600 °C) and annealing at varying temperature (700 to 1100 °C), time (up to 144 h) and stress (up to 1.5 GPa) were carried out in a Griggs-type apparatus on natural olivine-rich peridotite s
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3fb4bace5e57bf280cbfc1ac722a2421
https://doi.org/10.5194/se-4-423-2013
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6
Kick-and-cook experiments on peridotite: simulating coseismic deformation and post-seismic creep
Autor: Jörg Renner, Anthony Druiventak, Agnes Matysiak, Claudia A. Trepmann
Publikováno v: Terra Nova. 24:62-69
Terra Nova, 24, 62–69, 2012 Abstract Experiments comprising deformation at 600 °C and annealing at 700–1000 °C were performed on natural peridotite to examine the microfabric evolution at conditions corresponding to those prevailing just below
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::7d26650fb389a0abae533e542058b9d7
https://doi.org/10.1111/j.1365-3121.2011.01038.x
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7
Low-temperature plasticity of olivine during high stress deformation of peridotite at lithospheric conditions — An experimental study
Autor: Jörg Renner, Karin Hanke, Claudia A. Trepmann, Anthony Druiventak
Publikováno v: Earth and Planetary Science Letters. 311:199-211
Deformation experiments on natural peridotite from the Almklovdalen complex, Norway, were carried out in a Griggs-type apparatus at temperatures of 20, 300, and 600 °C, confining pressures of 1.0 to 2.5 GPa, and strain rates of 3·10 −6 to 8 · 10
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::8b0d73592ed6efc0cbadff5e6c212225
https://doi.org/10.1016/j.epsl.2011.09.022
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8
Case histories of hydraulic conductivity estimation with induced polarization at the field scale
Autor: Andreas Kemna, Andreas Hördt, P. Kreye, Norbert Zisser, F. Binot, R. Blaschek, A. Druiventak
Publikováno v: Near Surface Geophysics. 7:529-545
We have carried out spectral induced polarization (IP) measurements at three different hydrogeological test sites (Hasloh, Ludingworth and Kappelen) and estimated hydraulic conductivity using empirical equations previously derived from laboratory mea
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b9970f6cb5b63dfd260397d64d59a5bf
https://doi.org/10.3997/1873-0604.2009035
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10
Experimental deformation and recrystallization of olivine – processes and time scales of damage healing during postseismic relaxation at mantle depths
Autor: C. A. Trepmann, J. Renner, A. Druiventak
Experiments comprising sequences of deformation (at 300 or 600 °C) and annealing at varying temperature (700 to 1100 °C), time (up to 144 h) and stress (up to 1.5 GPa) were carried out in a Griggs-type apparatus on natural olivine-rich peridotite
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::53f6062850f6b7f3ac7f39dce6e1a6b2
https://doi.org/10.5194/sed-5-463-2013
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