| Frictional and hydrologic properties of clay‐rich fault gouge MJ Ikari, DM Saffer, C Marone Journal of Geophysical Research: Solid Earth 114 (B5), 2009 | 505 | 2009 |
| On the relation between fault strength and frictional stability MJ Ikari, C Marone, DM Saffer Geology 39 (1), 83-86, 2011 | 373 | 2011 |
| Low coseismic friction on the Tohoku-Oki fault determined from temperature measurements PM Fulton, EE Brodsky, Y Kano, J Mori, F Chester, T Ishikawa, RN Harris, ... Science 342 (6163), 1214-1217, 2013 | 335 | 2013 |
| Structure and composition of the plate-boundary slip zone for the 2011 Tohoku-Oki earthquake FM Chester, C Rowe, K Ujiie, J Kirkpatrick, C Regalla, F Remitti, ... Science 342 (6163), 1208-1211, 2013 | 305 | 2013 |
| Low coseismic shear stress on the Tohoku-Oki megathrust determined from laboratory experiments K Ujiie, H Tanaka, T Saito, A Tsutsumi, JJ Mori, J Kameda, EE Brodsky, ... Science 342 (6163), 1211-1214, 2013 | 297 | 2013 |
| Effect of hydration state on the frictional properties of montmorillonite‐based fault gouge MJ Ikari, DM Saffer, C Marone Journal of Geophysical Research: Solid Earth 112 (B6), 2007 | 236 | 2007 |
| Slip weakening as a mechanism for slow earthquakes MJ Ikari, C Marone, DM Saffer, AJ Kopf Nature geoscience 6 (6), 468-472, 2013 | 188 | 2013 |
| The thickness of subduction plate boundary faults from the seafloor into the seismogenic zone CD Rowe, JC Moore, F Remitti, IODP Expedition 343/343T Scientists Geology 41 (9), 991-994, 2013 | 150 | 2013 |
| Source of Oligocene to Pliocene sedimentary rocks in the Linxia basin in northeastern Tibet from Nd isotopes: Implications for tectonic forcing of climate CN Garzione, MJ Ikari, AR Basu Geological Society of America Bulletin 117 (9-10), 1156-1166, 2005 | 150 | 2005 |
| Stress state in the largest displacement area of the 2011 Tohoku-Oki earthquake W Lin, M Conin, JC Moore, FM Chester, Y Nakamura, JJ Mori, L Anderson, ... Science 339 (6120), 687-690, 2013 | 142 | 2013 |
| Slow slip source characterized by lithological and geometric heterogeneity PM Barnes, LM Wallace, DM Saffer, RE Bell, MB Underwood, A Fagereng, ... Science Advances 6 (13), eaay3314, 2020 | 130 | 2020 |
| Laboratory observations of time‐dependent frictional strengthening and stress relaxation in natural and synthetic fault gouges BM Carpenter, MJ Ikari, C Marone Journal of Geophysical Research: Solid Earth 121 (2), 1183-1201, 2016 | 119 | 2016 |
| Clay fabric intensity in natural and artificial fault gouges: Implications for brittle fault zone processes and sedimentary basin clay fabric evolution SH Haines, BA Van Der Pluijm, MJ Ikari, DM Saffer, C Marone Journal of Geophysical Research: Solid Earth 114 (B5), 2009 | 111 | 2009 |
| A microphysical interpretation of rate‐and state‐dependent friction for fault gouge MJ Ikari, BM Carpenter, C Marone Geochemistry, Geophysics, Geosystems 17 (5), 1660-1677, 2016 | 101 | 2016 |
| Cohesive strength of clay‐rich sediment MJ Ikari, AJ Kopf Geophysical research letters 38 (16), 2011 | 99 | 2011 |
| Comparison of frictional strength and velocity dependence between fault zones in the Nankai accretionary complex MJ Ikari, DM Saffer Geochemistry, Geophysics, Geosystems 12 (4), 2011 | 99 | 2011 |
| The role of fault zone fabric and lithification state on frictional strength, constitutive behavior, and deformation microstructure MJ Ikari, AR Niemeijer, C Marone Journal of Geophysical Research: Solid Earth 116 (B8), 2011 | 96 | 2011 |
| Pelagic smectite as an important factor in tsunamigenic slip along the Japan Trench J Kameda, M Shimizu, K Ujiie, T Hirose, M Ikari, J Mori, K Oohashi, ... Geology 43 (2), 155-158, 2015 | 85 | 2015 |
| The state of stress on the fault before, during, and after a major earthquake EE Brodsky, JJ Mori, L Anderson, FM Chester, M Conin, EM Dunham, ... Annual Review of Earth and Planetary Sciences 48 (1), 49-74, 2020 | 76 | 2020 |
| Frictional and hydrologic properties of a major splay fault system, Nankai subduction zone MJ Ikari, DM Saffer, C Marone Geophysical Research Letters 36 (20), 2009 | 76 | 2009 |
