80 citations as recorded by crossref.

1. Tectonic, climatic, and diagenetic control of magnetic properties of sediments from Kumano Basin, Nankai margin, southwestern Japan M. Shi et al.
2. Depositional architecture, provenance, and tectonic/eustatic modulation of Miocene submarine fans in the Shikoku Basin: Results from Nankai Trough Seismogenic Zone Experiment K. Pickering et al.
3. Slumping and mass transport deposition in the Nankai fore arc: Evidence from IODP drilling and 3‐D reflection seismic data M. Strasser et al.
4. Re-evaluation of temperature at the updip limit of locked portion of Nankai megasplay inferred from IODP Site C0002 temperature observatory T. Sugihara et al.
5. Implications of basement rock alteration in the Nankai Trough, Japan for subduction megathrust slip behavior M. Ikari et al.
6. Sequence stratigraphic evolution of the Kumano forearc basin during the last deglaciation: Influence of eustasy and tectonically-controlled shelf morphology on deep-marine sediment dynamics P. Cornard et al.
7. The permeability of active subduction plate boundary faults D. Saffer
8. In situ thermal excursions detected in the Nankai Trough forearc slope sediment at IODP NanTroSEIZE Site C0008 M. Kinoshita et al.
9. The effect of thermal pressurization on dynamic fault branching Y. Urata et al.
10. No evidence for an active margin-spanning megasplay fault at the Cascadia Subduction Zone M. Lucas et al.
11. Episodic deformation and inferred slow slip at the Nankai subduction zone during the first decade of CORK borehole pressure and VLFE monitoring E. Davis et al.
12. Tectonic Influences on Trench Slope Basin Development via Structural Restoration Along the Outer Nankai Accretionary Prism, Southwest Japan J. Lackey et al.
13. Fluid flow and water–rock interaction across the active Nankai Trough subduction zone forearc revealed by boron isotope geochemistry A. Hüpers et al.
14. Late Quaternary Surface Displacements on Accretionary Wedge Splay Faults in the Cascadia Subduction Zone: Implications for Megathrust Rupture A. Ledeczi et al.
15. Apparent overconsolidation of mudstones in the Kumano Basin of southwest Japan: Implications for fluid pressure and fluid flow within a forearc setting J. Guo et al.
16. Friction experiments under in-situ stress reveal unexpected velocity-weakening in Nankai accretionary prism samples A. Roesner et al.
17. Quantifying structural uncertainty on fault networks using a marked point process within a Bayesian framework O. Aydin & J. Caers
18. Rejuvenated extension of the Philippine Sea plate and its effect on subduction dynamics in the Nankai Trough G. Kimura et al.
19. Transport process of sand grains from fluvial to deep marine regions estimated by luminescence of feldspar: example from theKumano area, centralJapan M. Shirai & R. Hayashizaki
20. Linking Faults, Fractures, and Clay Mineral Occurrence With Fluid Transport in the Accretionary Prism of the Nankai Trough, Japan A. Schleicher & M. Jurado
21. Three-Dimensional Splay Fault Geometry and Implications for Tsunami Generation G. Moore et al.
22. Simulation of methane hydrate formation in coarse‐ to fine‐grained sediments in the Nankai Trough, Japan C. Xu & H. Tomaru
23. Estimation of slip rate and fault displacement during shallow earthquake rupture in the Nankai subduction zone Y. Hamada et al.
24. Strike-slip deformation reflects complex partitioning of strain in the Nankai Accretionary Prism (SE Japan) M. Azevedo et al.
25. Tectonic mélange as fault rock of subduction plate boundary G. Kimura et al.
26. Waveform tomography imaging of a megasplay fault system in the seismogenic Nankai subduction zone R. Kamei et al.
27. Sr, Nd, and Pb isotope compositions of hemipelagic sediment in the Shikoku Basin: Implications for sediment transport by the Kuroshio and Philippine Sea plate motion in the late Cenozoic Y. Saitoh et al.
28. Recent scientific and operational achievements of D/V Chikyu A. Taira et al.
29. The stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai Trough J. Bedford et al.
30. Structural and fabric analyses of basal slip zone of the Jin’nosuke-dani landslide, northern central Japan: its application to the slip mechanism of decollement K. Kawamura et al.
31. Mid-Quaternary decoupling of sediment routing in the Nankai Forearc revealed by provenance analysis of turbiditic sands M. Usman et al.
32. Direct constraints on in situ stress state from deep drilling into the Nankai subduction zone, Japan H. Tobin et al.
33. Combining Multisite Tsunami and Deformation Modeling to Constrain Slip Distributions for the 1700 C.E. Cascadia Earthquake D. Small et al.
34. Hydrocarbon seepage and its sources at mud volcanoes of the Kumano forearc basin, Nankai Trough subduction zone T. Pape et al.
35. Rheology and Biostratigraphy of the Mariana Serpentine Muds Unravel Mud Volcano Evolution W. Menapace et al.
36. Fluid budgets along the northern Hikurangi subduction margin, New Zealand: the effect of a subducting seamount on fluid pressure S. Ellis et al.
37. Mechanical Weakness of the Nankai Accretionary Prism: Insights From Vp Measurements of Drill Cuttings M. Kitamura et al.
38. Stress reversal recorded in calcite vein cuttings from the Nankai accretionary prism, southwest Japan T. Takeshita et al.
39. Origin and in situ concentrations of hydrocarbons in the Kumano forearc basin from drilling mud gas monitoring during IODP NanTroSEIZE Exp. 319 T. Wiersberg et al.
40. Longitudinal natural vibration of ultra-long drill string during offshore drilling R. Wada et al.
41. Hanging wall deformation of a seismogenic megasplay fault in an accretionary prism: The Nobeoka Thrust in southwestern Japan G. Kimura et al.
42. PandSwave velocity measurements of water-rich sediments from the Nankai Trough, Japan K. Schumann et al.
43. Imaging deformation in submarine thrust belts using seismic attributes D. Iacopini & R. Butler
44. Characteristics of a tsunamigenic megasplay fault in the Nankai Trough Y. Yamada et al.
45. Crustal Structure of the Nankai Subduction Zone Revealed by Two Decades of Onshore‐Offshore and Ocean‐Bottom Seismic Data: Implications for the Dimensions and Slip Behavior of the Seismogenic Zone D. Bassett et al.
46. Punctuated growth of an accretionary prism and the onset of a seismogenic megathrust in the Nankai Trough G. Kimura et al.
47. In Situ Stress and Pore Pressure in the Deep Interior of the Nankai Accretionary Prism, Integrated Ocean Drilling Program Site C0002 H. Kitajima et al.
48. Sedimentary inputs to the Nankai subduction zone: The importance of dispersed ash R. Scudder et al.
49. Fault strength, healing and stability in the Nankai Trough accretionary prism off Kii Peninsula, Japan, as illustrated by friction experiments on gouge of a cored sample K. Kanagawa et al.
50. Sediment provenance, routing and tectonic linkages in the Nankai forearc region, Japan S. Ramirez et al.
51. Shear behavior of DFDP-1 borehole samples from the Alpine Fault, New Zealand, under a wide range of experimental conditions M. Ikari et al.
52. Projection of mechanical properties from shallow to greater depths seaward of the Nankai accretionary prism M. Ask & J. Morgan
53. Layered anisotropy within the crust and lithospheric mantle beneath the Sea of Japan C. Legendre et al.
54. Present‐day stress states underneath the Kumano basin to 2 km below seafloor based on borehole wall failures at IODP site C0002, Nankai accretionary wedge C. Chang & I. Song
55. Clay-mineral assemblages across the Nankai-Shikoku subduction system, offshore Japan: A synthesis of results from the NanTroSEIZE project M. Underwood & J. Guo
56. Strain decoupling reveals variable seismogenic risk in SEJapan (Nankai Trough) J. Van Tuyl et al.
57. Depositional age and triggering event of turbidites in the western Kumano Trough, central Japan during the last ca. 100 years M. Shirai et al.
58. Long-distance fluid and heat transport in the oceanic crust entering the Nankai subduction zone, NanTroSEIZE transect G. Spinelli
59. Submarine landslide potential near the megasplay fault at the Nankai subduction zone M. Ikari et al.
60. Paleocurrent analysis of Pleistocene turbidite sediments in the forearc basin inferred from anisotropy of magnetic susceptibility and paleomagnetic data at the gas hydrate production test site in the eastern Nankai Trough M. Tamaki et al.
61. Evolution of sediment permeability during burial and subduction H. Daigle & E. Screaton
62. Strength Profile of the Inner Nankai Accretionary Prism at IODP Site C0002 M. Kitamura et al.
63. Microporosity development in shallow marine sediments from the Nankai Trough H. Daigle
64. Elevated fluid pressure and extreme mechanical weakness of a plate boundary thrust, Nankai Trough subduction zone H. Tobin & D. Saffer
65. Large volume submarine ignimbrites in the Shikoku Basin: An example for explosive volcanism in the Western Pacific during the Late Miocene S. Kutterolf et al.
66. Geochemical approaches to the quantification of dispersed volcanic ash in marine sediment R. Scudder et al.
67. Pore pressure development beneath the décollement at the Nankai subduction zone: Implications for plate boundary fault strength and sediment dewatering R. Skarbek & D. Saffer
68. 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 O. Fabbri et al.
69. Tsunami hazard analysis for Chinese coast from potential earthquakes in the western North Pacific J. Hou et al.
70. Structural styles across the Nankai accretionary prism revealed from LWD borehole images and their correlation with seismic profile and core data: Results from NanTroSEIZE Stage 1 expeditions Y. Yamada et al.
71. Structural evolution of an inner accretionary wedge and forearc basin initiation, Nankai margin, Japan N. Hayman et al.
72. Erosional features as indicators of thrust fault activity (Nankai Trough, Japan) T. Alves et al.
73. Shear strength of sediments approaching subduction in the Nankai Trough, Japan as constraints on forearc mechanics M. Ikari et al.
74. Effective strength of incoming sediments and its implications for plate boundary propagation: Nankai and Costa Rica as type examples of accreting vs. erosive convergent margins A. Kopf
75. Origin and evolution of a splay fault in the Nankai accretionary wedge M. Strasser et al.
76. Misfit functionals in Laplace‐Fourier domain waveform inversion, with application to wide‐angle ocean bottom seismograph data R. Kamei et al.
77. Multiple sub-parallel seismogenic zones at the upper fringe of the aftershock zone of the M5.5 Orkney earthquake, South Africa K. Fujita et al.
78. On acoustic waveform tomography of wide-angle OBS data--strategies for pre-conditioning and inversion R. Kamei et al.
79. The role of mud volcanism and deep‐seated dewatering processes in the Nankai Trough accretionary prism and Kumano Basin, Japan W. Menapace et al.
80. Seismic Anisotropy and Its Impact on Imaging the Shallow Alpine Fault: An Experimental and Modeling Perspective L. Adam et al.