Year |
Citation |
Score |
2020 |
Barnes PM, Wallace LM, Saffer DM, Bell RE, Underwood MB, Fagereng A, Meneghini F, Savage HM, Rabinowitz HS, Morgan JK, Kitajima H, Kutterolf S, Hashimoto Y, Engelmann de Oliveira CH, Noda A, ... ... Screaton EJ, et al. Slow slip source characterized by lithological and geometric heterogeneity. Science Advances. 6: eaay3314. PMID 32232148 DOI: 10.1126/Sciadv.Aay3314 |
0.311 |
|
2020 |
Fabbri O, Goldsby DL, Chester F, Karpoff AM, Morvan G, Ujiie K, Yamaguchi A, Sakaguchi A, Li CF, Kimura G, Tsutsumi A, Screaton E, Curewitz D. Deformation structures from splay and décollement faults in the Nankai accretionary prism, SW Japan (IODP NanTroSEIZE Expedition 316). Evidence for slow and rapid slip in fault rocks Geochemistry Geophysics Geosystems. 21. DOI: 10.1029/2019Gc008786 |
0.311 |
|
2019 |
Riedinger N, Torres M, Screaton E, Solomon E, Kutterolf S, Schindlbeck‐Belo J, Formolo M, Lyons T, Vannucchi P. Interplay of Subduction Tectonics, Sedimentation, and Carbon Cycling Geochemistry, Geophysics, Geosystems. 20: 4939-4955. DOI: 10.1029/2019Gc008613 |
0.402 |
|
2017 |
Hamahashi M, Screaton E, Tanikawa W, Hashimoto Y, Martin K, Saito S, Kimura G. Normal faulting and mass movement during ridge subduction inferred from porosity transition and zeolitization in the Costa Rica subduction zone Geochemistry Geophysics Geosystems. 18: 2601-2616. DOI: 10.1002/2016Gc006577 |
0.518 |
|
2013 |
Gulley J, Martin J, Spellman P, Moore P, Screaton E. Dissolution in a variably confined carbonate platform: effects of allogenic runoff, hydraulic damming of groundwater inputs, and surface–groundwater exchange at the basin scale Earth Surface Processes and Landforms. 38: 1700-1713. DOI: 10.1002/Esp.3411 |
0.445 |
|
2012 |
Marcaillou B, Henry P, Kinoshita M, Kanamatsu T, Screaton E, Daigle H, Harcouët-Menou V, Lee Y, Matsubayashi O, Kyaw Thu M, Kodaira S, Yamano M. Seismogenic zone temperatures and heat-flow anomalies in the To-nankai margin segment based on temperature data from IODP expedition 333 and thermal model Earth and Planetary Science Letters. 349: 171-185. DOI: 10.1016/J.Epsl.2012.06.048 |
0.359 |
|
2011 |
Gamage K, Screaton E, Bekins B, Aiello I. Permeability-porosity relationships of subduction zone sediments Marine Geology. 279: 19-36. DOI: 10.1016/J.Margeo.2010.10.010 |
0.538 |
|
2009 |
Tobin H, Kinoshita M, Ashi J, Lallemant S, Kimura G, Screaton E, Thu MK, Masago H, Curewitz D, Expeditions I, Party S. NanTroSEIZE Stage 1 Expeditions 314, 315, and 316: First Drilling Program of the Nankai Trough Seismogenic Zone Experiment Scientific Drilling. 8: 4-17. DOI: 10.2204/Iodp.Sd.8.01.2009 |
0.315 |
|
2009 |
Screaton E, Kimura G, Curewitz D, Moore G, Chester F, Fabbri O, Fergusson C, Girault F, Goldsby D, Harris R, Inagaki F, Jiang T, Kitamura Y, Knuth M, Li CF, et al. Interactions between deformation and fluids in the frontal thrust region of the NanTroSEIZE transect offshore the Kii Peninsula, Japan: Results from IODP Expedition 316 Sites C0006 and C0007 Geochemistry, Geophysics, Geosystems. 10. DOI: 10.1029/2009Gc002713 |
0.505 |
|
2009 |
Gulley JD, Benn DI, Screaton E, Martin J. Mechanisms of englacial conduit formation and their implications for subglacial recharge Quaternary Science Reviews. 28: 1984-1999. DOI: 10.1016/J.Quascirev.2009.04.002 |
0.425 |
|
2006 |
Screaton E. Excess pore pressures within subducting sediments: Does the proportion of accreted versus subducted sediments matter? Geophysical Research Letters. 33. DOI: 10.1029/2006Gl025737 |
0.673 |
|
2006 |
Gamage K, Screaton E. Characterization of excess pore pressures at the toe of the Nankai accretionary complex, Ocean Drilling Program sites 1173, 1174, and 808: Results of one-dimensional modeling Journal of Geophysical Research: Solid Earth. 111. DOI: 10.1029/2004Jb003572 |
0.537 |
|
2005 |
Ge S, Screaton E. Modeling seismically induced deformation and fluid flow in the Nanki subduction zone Geophysical Research Letters. 32: 1-4. DOI: 10.1029/2005Gl023473 |
0.56 |
|
2004 |
Screaton E, Martin JB, Ginn B, Smith L. Conduit properties and karstification in the unconfined Floridan aquifer. Ground Water. 42: 338-46. PMID 15161151 DOI: 10.1111/J.1745-6584.2004.Tb02682.X |
0.314 |
|
2003 |
Ge S, Bekins B, Bredehoeft J, Brown K, Davis EE, Gorelick SM, Henry P, Kooi H, Moench AF, Ruppel C, Sauter M, Screaton E, Swart PK, Tokunaga T, Voss CI, et al. Fluid flow in sub-sea floor processes and future ocean drilling Eos. 84: 145+151-152. DOI: 10.1029/2003Eo160002 |
0.411 |
|
2002 |
Screaton E, Saffer D, Henry P, Hunze S. Porosity loss within the underthrust sediments of the Nankai accretionary complex: Implications for overpressures Geology. 30: 19-22. DOI: 10.1130/0091-7613(2002)030<0019:Plwtus>2.0.Co;2 |
0.614 |
|
2000 |
Screaton E, Carson B, Davis E, Becker K. Permeability of a decollement zone: Results from a two-well experiment in the Barbados accretionary complex Journal of Geophysical Research. 105: 21403-21410. DOI: 10.1029/2000Jb900220 |
0.515 |
|
2000 |
Screaton E, Ge S. Anomalously high porosities in the proto-decollement zone of the Barbados accretionary complex: Do they indicate overpressures? Geophysical Research Letters. 27: 1993-1996. DOI: 10.1029/1999Gl011240 |
0.618 |
|
1997 |
McAdoo BG, Orange DL, Screaton E, Lee H, Kayen R. Slope basins, headless canyons, and submarine palaeoseismology of the Cascadia accretionary complex Basin Research. 9: 313-324. DOI: 10.1046/J.1365-2117.1997.00049.X |
0.505 |
|
1997 |
Orange DL, McAdoo BG, Moore JC, Tobin H, Screaton E, Chezar H, Lee H, Reid M, Vail R. Headless submarine canyons and fluid flow on the toe of the Cascadia accretionary complex Basin Research. 9: 303-312. DOI: 10.1046/J.1365-2117.1997.00045.X |
0.461 |
|
1997 |
Screaton E, Ge S. An assessment of along-strike fluid and heat transport within the Barbados Ridge accretionary complex: Results of preliminary modeling Geophysical Research Letters. 24: 3085-3088. DOI: 10.1029/97Gl03097 |
0.49 |
|
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