Year |
Citation |
Score |
2013 |
Kneller EA, Albertz M, Karner GD, Johnson CA. Testing inverse kinematic models of paleocrustal thickness in extensional systems with high-resolution forward thermo-mechanical models Geochemistry, Geophysics, Geosystems. 14: 2383-2398. DOI: 10.1002/Ggge.20153 |
0.58 |
|
2012 |
Kneller EA, Johnson CA, Karner GD, Einhorn J, Queffelec TA. Inverse methods for modeling non-rigid plate kinematics: Application to mesozoic plate reconstructions of the Central Atlantic Computers & Geosciences. 49: 217-230. DOI: 10.1016/J.Cageo.2012.06.019 |
0.494 |
|
2008 |
Kneller EA, van Keken PE. Effect of three-dimensional slab geometry on deformation in the mantle wedge: Implications for shear wave anisotropy Geochemistry, Geophysics, Geosystems. 9: n/a-n/a. DOI: 10.1029/2007Gc001677 |
0.689 |
|
2008 |
Kneller EA, Long MD, van Keken PE. Olivine fabric transitions and shear wave anisotropy in the Ryukyu subduction system Earth and Planetary Science Letters. 268: 268-282. DOI: 10.1016/J.Epsl.2008.01.004 |
0.678 |
|
2007 |
Kneller EA, van Keken PE. Trench-parallel flow and seismic anisotropy in the Mariana and Andean subduction systems. Nature. 450: 1222-5. PMID 18097407 DOI: 10.1038/Nature06429 |
0.689 |
|
2007 |
Kneller EA, van Keken PE, Katayama I, Karato S. Stress, strain, and B-type olivine fabric in the fore-arc mantle: Sensitivity tests using high-resolution steady-state subduction zone models Journal of Geophysical Research: Solid Earth. 112. DOI: 10.1029/2006Jb004544 |
0.701 |
|
2006 |
Abers GA, van Keken PE, Kneller EA, Ferris A, Stachnik JC. The thermal structure of subduction zones constrained by seismic imaging: Implications for slab dehydration and wedge flow Earth and Planetary Science Letters. 241: 387-397. DOI: 10.1016/J.Epsl.2005.11.055 |
0.656 |
|
2005 |
Kneller EA, van Keken PE, Karato S, Park J. B-type olivine fabric in the mantle wedge: Insights from high-resolution non-Newtonian subduction zone models Earth and Planetary Science Letters. 237: 781-797. DOI: 10.1016/J.Epsl.2005.06.049 |
0.672 |
|
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